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A simple model for estimation of above and below ground carbon in cereal crops

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  • Carbon (C) is an essential part of healthy soil. Healthy soils play an important role in improving the life of all living organisms on earth (plants, humans, animals, birds, insects, microbes etc.). Best agronomic practices for field crop production sequester more carbon (due to higher photosynthesis) below and above the ground that makes the soils healthy and sustainable. Healthy soils increase yield per unit area and so reduce the problem of food insecurity. Higher photosynthetic efficiency (higher CO2 uptake by the plants) reduces the problem of global warming and climate change. According to an estimate, plants capture about 860 gigatons of CO2 each year from the atmosphere, storing it in their shoots, and roots (1 kg of carbon is equal to 3.67 kg of CO2). The aim of this study was to develop a simple calculation (model) for researchers to easily estimate the carbon content (CC) capture by plants in below (roots) and above ground (shoots) parts. Considerable variation in total CC (TCC) accumulation and its partitioning into above ground parts (ACC) and below ground parts (BCC) exists which depends on crop species and genotypes, crop nutrition, crop competitions and intercropping, fertilizers application, irrigation, tillage, biotic and abiotic stresses, soil types and environment etc. The CC estimation is explained in detail with four examples on major cereal crops (wheat, rice, maize and barley) for the world leading countries in 2018−2019. In the first example using wheat, the TCC estimated for wheat crop in Pakistan was 37.4 metric tons (MT) of which 30.5 MT was allocated into ACC (shoots) and 6.9 MT into BCC (roots). The highest value of TCC accumulation for wheat crop was estimated for the European Union which was 216.3 MT (176.4 ACC + 39.9 BCC). In the second example using rice crop, TCC for the world leading countries was estimated and the leading country was China with TCC of 161.7 MT (131.9 ACC + 29.8 BCC). Example three is about the CC estimation for maize crop, and the leading country was USA having the highest TCC value of 505.3 MT (ACC = 412.1 MT, BCC = 93.2 MT). The Russian Federation ranked first for barley crop and the highest TCC value of 29.2 MT was recorded (23.8 MT ACC + 5.4 MT BCC). It was confirmed while using this model that out of the 100% (TCC) fixed, about 82% CC is partitioned into above ground parts (ACC) and the remaining 18% CC is allocated into below ground parts (BCC). Due to this model, we can easily calculate the TCC accumulation and its partitioning into ACC and BCC per unit area (kg·ha−1). For example, the TCC was easily calculated for the 40 world leading countries for wheat, rice, maize and barley during 2019. The results revealed that the TCC ranged from 4,414 to 13,243 kg·ha−1 for wheat, 4,578 to 11,444 kg·ha−1 for rice, 5,150 to 15,450 kg·ha1 for maize, and 3,443 to 13,733 kg·ha−1 for barley among the top 40 countries. This is the most simplified approach for estimating carbon content in the below-ground (roots) and above-ground (shoots) parts of field crops.
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  • [1]

    Amanullah. 2018. Best Management Practices Reduce Soil Pollution and Improve Health of All: a review. Proceeding of the Global symposium on soil pollution held at UN FAO Headquarters- Rome, Italy, 2−4 May, 2018. pp: 262−67

    [2]

    Amanullah, Iqbal A, Khan A, Khalid S, Shah A, et al. 2019. Integrated management of phosphorus, organic sources, and beneficial microbes improve dry matter partitioning of maize. Communications in Soil Science and Plant Analysis 50:2544−69

    doi: 10.1080/00103624.2019.1667378

    CrossRef   Google Scholar

    [3]

    Amanullah, Inamullah, Alkahtani J, Elshikh MS, Alwahibi MS, et al. 2020. Phosphorus and zinc fertilization influence crop growth rates and total biomass of coarse vs. fine types rice cultivars. Agronomy 10:1356

    doi: 10.3390/agronomy10091356

    CrossRef   Google Scholar

    [4]

    Amanullah, Khalid S, Khalil F, Elshikh MS, Alwahibi MS, et al. 2021. Growth and dry matter partitioning response in cereal-legume intercropping under full and limited irrigation regimes. Scientific Reports 11:12585

    doi: 10.1038/s41598-021-92022-4

    CrossRef   Google Scholar

    [5]

    Kruger EL, Volin JC. 2006. Reexamining the empirical relation between plant growth and leaf photosynthesis. Functional Plant Biology 33:421

    doi: 10.1071/fp05310

    CrossRef   Google Scholar

    [6]

    Irving LJ. 2015. Carbon assimilation, biomass partitioning and productivity in grasses. Agriculture 5:1116−34

    doi: 10.3390/agriculture5041116

    CrossRef   Google Scholar

    [7]

    IPCC. 2014. Climate Change 2014: Synthesis, Report Contribution of Working Groups I, II and III to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Geneva, IPCC. 104 pp.

    [8]

    FAO. 2019a. Measuring and modelling soil carbon stocks and stock changes in livestock production systems – Guidelines for assessment. Version 1. Advanced copy. 152 pp.

    [9]

    FAO. 2019b. Measuring and modelling soil carbon stocks and stock changes in livestock production systems – A scoping analysis for the LEAP work stream on soil carbon stock changes. Rome. 84 pp. https://www.fao.org/3/CA2933EN/ca2933en.pdf

    [10]

    FAO. 2019c. The international code of conduct for the sustainable use and management of fertilizers. Rome, FAO. 30 pp.

    [11]

    FAO Outlook. 2018. Biannual report on global food markets. Rome, FAO.

    [12]

    FAO. 2017a. Unlocking the Potential of Soil Organic Carbon. FAO, IPCC, UNCCD, UNO, WMO.

    [13]

    FAO. 2017b. Proceedings of the Global Symposium on Soil Organic Carbon. FAO, Rome, Italy

    [14]

    FAO. 2017c. Soil Organic Carbon: the hidden potential. FAO, Rome, Italy

    [15]

    UNFCCC. 2014. Handbook on Measurement, Reporting and Verification for developing countries. Bonn

    [16]

    IPBES. 2015. Scoping for a thematic assessment of land degradation and restoration (deliverable 3(b) (i)). www.ipbes.net/event/ipbes-3-plenary

    [17]

    Eggleston HS, Buendia L, Miwa K, Ngara T, Tanabe K. (Eds.). 2006. IPCC guidelines for national greenhouse gas inventories. IGES, Japan. National Greenhouse Gas Inventories Programme.

    [18]

    UNEP, SETAC. 2011. Global guidance principles for life cycle assessment databases. www.unep.org/pdf/Global-Guidance-Principles-for-LCA.pdf

    [19]

    Chen S, Wang W, Xu W, Wang Y, Wan H, et al. 2018. Plant diversity enhances productivity and soil carbon storage. Proceedings of the National Academy of Sciences of the United States of America 115:4027−32

    doi: 10.1073/pnas.1700298114

    CrossRef   Google Scholar

    [20]

    Davis MR, Alves BJR, Karlen DL, Kline KL, Galdos M, Abulebdeh D. 2018. Review of soil organic carbon measurement protocols: A US and Brazil comparison and recommendation. Sustainability 10:53

    doi: 10.3390/su10010053

    CrossRef   Google Scholar

    [21]

    Ma S, He F, Tian D, Zou D, Yan Z, et al. 2018. Variations and determinants of carbon content in plants: a global synthesis. Biogeosciences 15:693−702

    doi: 10.5194/bg-15-693-2018

    CrossRef   Google Scholar

    [22]

    Malone B, Hedley C, Roudier P, Minasny B, Jones E, et al. 2018. Auditing on-farm soil carbon stocks using downscaled national mapping products: examples from Australia and New Zealand. Geoderma 13:1−14

    doi: 10.1016/j.geodrs.2018.02.002

    CrossRef   Google Scholar

    [23]

    Bispo A, Andersen L, Angers DA, Bernoux M, Brossard M, et al. 2017. Accounting for carbon stocks in soils and measuring GHGs emission fluxes from soils: do we have the necessary standards? Frontiers in Environmental Science 5:41

    doi: 10.3389/fenvs.2017.00041

    CrossRef   Google Scholar

    [24]

    Brilli L, Bechini L, Bindi M, Carozzi M, Cavalli D, et al. 2017. Review and analysis of strengths and weaknesses of agro-ecosystem models for simulating C and N fluxes. The Science of the Total Environment 598:445−70

    doi: 10.1016/j.scitotenv.2017.03.208

    CrossRef   Google Scholar

    [25]

    Chevallier T, Cournac L, Bernoux M, Cardinael R, Cozzi T, et al. 2017. Soil inorganic carbon and climate change in drylands. An emerging issue? Proceedings of the Global Symposium on Soil Organic Carbon. FAO, Rome, Italy. pp: 482−85

    [26]

    Conrad KA, Dalal RC, Dalzell SA, Allen DE, Menzies NW. 2017. The sequestration and turnover of soil organic carbon in subtropical Leucaena-grass pastures. Agriculture, Ecosystems & Environment 248:38−47

    doi: 10.1016/j.agee.2017.07.020

    CrossRef   Google Scholar

    [27]

    Dignac MF, Derrien D, Barré P, Barot S, Cécillon L, et al. 2017. Increasing soil carbon storage: mechanisms, effects of agricultural practices and proxies. A review. Agronomy for Sustainable Development 37:14

    doi: 10.1007/s13593-017-0421-2

    CrossRef   Google Scholar

    [28]

    Maillard É, McConkey BG, Angers DA. 2017. Increased uncertainty in soil carbon stock measurement with spatial scale and sampling profile depth in world grasslands: a systematic analysis. Agriculture, Ecosystems & Environment 236:268−76

    doi: 10.1016/j.agee.2016.11.024

    CrossRef   Google Scholar

    [29]

    Jiang Q, Li Q, Wang X, Wu Y, Yang X, et al. 2017. Estimation of soil organic carbon and total nitrogen in different soil layers using VNIR spectroscopy: effects of spiking on model applicability. Geoderma 293:54−63

    doi: 10.1016/j.geoderma.2017.01.030

    CrossRef   Google Scholar

    [30]

    Stahl C, Fontaine S, Klumpp K, Picon-Cochard C, Grise MM, et al. 2017. Continuous soil carbon storage of old permanent pastures in Amazonia. Global Change Biology 23:3382−92

    doi: 10.1111/gcb.13573

    CrossRef   Google Scholar

    [31]

    Stahl C, Freycon V, Fontaine S, Dezécache C, Ponchant L, et al. 2016. Soil carbon stocks after conversion of Amazonian tropical forest to grazed pasture: importance of deep soil layers. Regional Environmental Change 16:2059−69

    doi: 10.1007/s10113-016-0936-0

    CrossRef   Google Scholar

    [32]

    Guo L, Zhao C, Zhang H, Chen Y, Linderman M, et al. 2017. Comparisons of spatial and non-spatial models for predicting soil carbon content based on visible and near-infrared spectral technology. Geoderma 285:280−92

    doi: 10.1016/j.geoderma.2016.10.010

    CrossRef   Google Scholar

    [33]

    Allen DE, Pringle MJ, Butler DW, Henry BK, Bishop TFA, et al. 2016. Effects of land-use change and management on soil carbon and nitrogen in the Brigalow Belt, Australia: I. Overview and inventory. The Rangeland Journal 38:443−52

    doi: 10.1071/rj16009

    CrossRef   Google Scholar

    [34]

    Carolan R, Fornara DA. 2016. Soil carbon cycling and storage along a chronosequence of re-seeded grasslands: do soil carbon stocks increase with grassland age? Agriculture, Ecosystems & Environment 218:126−32

    doi: 10.1016/J.AGEE.2015.11.021

    CrossRef   Google Scholar

    [35]

    Clairotte M, Grinand C, Kouakoua E, Thébault A, Saby NPA, et al. 2016. National calibration of soil organic carbon concentration using diffuse infrared reflectance spectroscopy. Geoderma 276:41−52

    doi: 10.1016/j.geoderma.2016.04.021

    CrossRef   Google Scholar

    [36]

    Fornara DA, Wasson EA, Christie P, Watson CJ. 2016. Long-term nutrient fertilization and the carbon balance of permanent grassland: any evidence for sustainable intensification? Biogeosciences 13:4975−84

    doi: 10.5194/bg-2016-224

    CrossRef   Google Scholar

    [37]

    Poeplau C. 2016. Estimating root: shoot ratio and soil carbon inputs in temperate grasslands with the RothC model. Plant and Soil 407:293−305

    doi: 10.1007/s11104-016-3017-8

    CrossRef   Google Scholar

    [38]

    de Souza DM, de Oliveira Morais PA, Matsushige I, Rosa LA. 2016. Development of alternative methods for determining soil organic matter. Revista Brasileira De Ciência Do Solo 40:e0150150

    doi: 10.1590/18069657rbcs20150150

    CrossRef   Google Scholar

    [39]

    McNally SR, Laughlin DC, Rutledge S, Dodd MB, Six J, et al. 2015. Root carbon inputs under moderately diverse sward and conventional ryegrass-clover pasture: implications for soil carbon sequestration. Plant and Soil 392:289−99

    doi: 10.1007/s11104-015-2463-z

    CrossRef   Google Scholar

    [40]

    Henry BK, Butler D, Wiedemann SG. 2015. Quantifying carbon sequestration on sheep grazing land in Australia for life cycle assessment studies. The Rangeland Journal 37:379−88

    doi: 10.1071/rj14109

    CrossRef   Google Scholar

    [41]

    Smith P. 2014. Do grasslands act as a perpetual sink for carbon? Global Change Biology 20:2708−11

    doi: 10.1111/gcb.12561

    CrossRef   Google Scholar

    [42]

    Skinner RH, Dell CJ. 2014. Comparing pasture C sequestration estimated from eddy covariance and soil cores. Agriculture, Ecosystems and Environment 199:52−57

    doi: 10.1016/j.agee.2014.08.020

    CrossRef   Google Scholar

    [43]

    Pringle MJ, Allen DE, Dalal RC, Payne JE, Mayer DG, et al. 2011. Soil carbon stock in the tropical rangelands of Australia: effects of soil type and grazing pressure, and determination of sampling requirement. Geoderma 167−168:261−73

    doi: 10.1016/j.geoderma.2011.09.001

    CrossRef   Google Scholar

    [44]

    Powlson DS, Whitmore AP, Goulding KWT. 2011. Soil carbon sequestration to mitigate climate change: a critical re-examination to identify the true and the false. European Journal of Soil Science 62:42−55

    doi: 10.1111/j.1365-2389.2010.01342.x

    CrossRef   Google Scholar

    [45]

    Amanullah. 2014. Wheat and rye differ in drymatter partitioning, shoot-root ratio and water use efficiency under organic and inorganic soils. Journal of Plant Nutrition 37:1885−97

    doi: 10.1080/01904167.2014.911888

    CrossRef   Google Scholar

    [46]

    Amanullah, Stewart BA, Ullah H. 2015. Cool season C3-grasses (wheat, rye, barley, and oats) differ in shoot: root ratio when applied with different NPK sources. Journal of Plant Nutrition 38:189−201

    doi: 10.1080/01904167.2014.881877

    CrossRef   Google Scholar

    [47]

    Amanullah, Khan S, Muhammad A. 2015. Beneficial microbes and phosphorus management influence dry matter partitioning and accumulation in wheat (Triticum aestivum L.) with and without moisture stress condition. Journal of Microbial & Biochemical Technology 7:410−416

    doi: 10.4172/1948-5948.1000247

    CrossRef   Google Scholar

    [48]

    Bert D, Danjon F. 2006. Carbon concentration variations in the roots, stem and crown of mature Pinus pinaster (Ait.). Forest Ecology and Management 222:279−95

    doi: 10.1016/j.foreco.2005.10.030

    CrossRef   Google Scholar

    [49]

    Yao F, Chen Y, Yan Z, Li P, Han W, et al. 2015. Biogeographic patterns of structural traits and C: N: P stoichiometry of tree twigs in China's forests. PLoS One 10:e0116391

    doi: 10.1371/journal.pone.0116391

    CrossRef   Google Scholar

    [50]

    Poorter H, Niklas KJ, Reich PB, Oleksyn J, Poot P, et al. 2012. Biomass allocation to leaves, stems and roots: meta-analyses of interspecific variation and environmental control. New Phytologist 193:30−50

    doi: 10.1111/j.1469-8137.2011.03952.x

    CrossRef   Google Scholar

    [51]

    Amanullah, Stewart BA, Almas LK. 2016. Root: shoot ratio and water use efficiency differ in cool season cereals grown in pure and mixed stands under low and high water levels. The Texas Journal of Agriculture and Natural Resources 29:52−65

    Google Scholar

    [52]

    Nadia, Amanullah, Arif M, Muhammad D. 2023. Improvement in wheat productivity with integrated management of beneficial microbes along with organic and inorganic phosphorus sources. Agriculture 13(6):1118

    doi: 10.3390/agriculture13061118

    CrossRef   Google Scholar

    [53]

    Amanullah, Asif M, Khan A, Khalid S. 2019. Integrated management of phosphorus, organic sources, and beneficial microbes improve dry matter partitioning of maize. Communications in Soil Science and Plant Analysis 50(20):2544−69

    Google Scholar

    [54]

    Redin M, Recous S, Aita C, Chaves B, Pfeifer IC, et al. 2018. Root and shoot contributionto carbon and nitrogen inputsin the topsoil layer in no-tillagecrop systems under subtropicalconditions. Rev Bras Cienc Solo 42:e0170355

    Google Scholar

    [55]

    Amanullah, Inamullah. 2016. Dry matter partitioning and harvest index differ in rice genotypes with variable rates of phosphorus and zinc nutrition. Rice Science 23(2):78−87

    doi: 10.1016/j.rsci.2015.09.006

    CrossRef   Google Scholar

    [56]

    Roumet C, Lafont F, Sari M, Warembourg F, Garnier E. 2008. Root traits and taxonomic affiliation of nine herbaceous species grown in glasshouse conditions. Plant and Soil 312:69−83

    doi: 10.1007/s11104-008-9635-z

    CrossRef   Google Scholar

    [57]

    Uri V, Varik M, Aosaar J, Kanal A, Kukumägi M, et al. 2012. Biomass production and carbon sequestration in a fertile silver birch (Betula pendula Roth) forest chronosequence. Forest Ecology and Management 267:117−26

    doi: 10.1016/j.foreco.2011.11.033

    CrossRef   Google Scholar

    [58]

    Martin AR, Thomas SC, Zhao Y. 2013. Size-dependent changes in wood chemical traits: a comparison of neotropical saplings and large trees. AoB PLANTS 5:plt039

    doi: 10.1093/aobpla/plt039

    CrossRef   Google Scholar

    [59]

    Amanullah, Stewart BA. 2015. Analysis of growth response of cool season cereals "wheat vs. rye" grown in organic and inorganic soils. Emirates Journal of Food and Agriculture 27:430

    doi: 10.9755/ejfa.2015.04.041

    CrossRef   Google Scholar

    [60]

    Amanullah, Shah S, Shah Z, Khalail SK, Jan A, et al. 2014. Effects of variable nitrogen source and rate on leaf area index and total dry matter accumulation in maize (Zea mays L.) genotypes under calcareous so. Turkish Journal of Field Crops 19:276−84

    Google Scholar

    [61]

    Amanullah, Stewart BA. 2013. Shoot: root differs in warm season c4-cereals when grown alone in pure and mixed stands under low and high water levels. Pakistan Journal of Botany 45:83−90

    Google Scholar

    [62]

    Bagrintseva VN, Nosov VV. 2012. Potassium nutrition for small grains grown on chestnut soils. Better Crops With Plant Food 96:29−31

    Google Scholar

    [63]

    Mut Z, Ayan K, Mut H. 2006. Evaluation of forage yield and quality at two phenological stages of triticale genotypes and other cereals grown under rainfed conditions. Bangladesh Journal of Botany 35:45−53

    Google Scholar

    [64]

    Amanullah, Khalid S, Imran, Khan HA, Arif M, et al. 2019. Organic Matter Management in Cereals Based System: Symbiosis for Improving Crop Productivity and Soil Health. In Sustainable Agriculture Reviews 29, eds. Lal R, Francaviglia R. Springer, Cham. pp. 67−92. https://doi.org/10.1007/978-3-030-26265-5_3

    [65]

    Amanullah, Hidayatullah, Jan A, Shah Z, Parmar B, et al. 2019. Organic carbon sources and nitrogen management improve biomass of hybrid rice (Oryza sativa L.) under nitrogen deficient condition. In Advances in Rice Research for Abiotic Stress Tolerance, eds. Hasanuzzaman M, Fujita M, Nahar K, Biswas JK. Chennai: Woodhead Publishing. pp: 447−68. https://doi.org/10.1016/B978-0-12-814332-2.00022-8

    [66]

    Amanullah. 2017. Effects of NPK source on the dry matter partitioning in cool season C3-cereals (wheat, rye, barley, and oats) at various growth stages. Journal of Plant Nutrition 40:352−64

    doi: 10.1080/01904167.2016.1240195

    CrossRef   Google Scholar

    [67]

    Amanullah, Stewart BA. 2013. Dry matter partitioning, growth analysis and water use efficiency response of oats (Avena sativa L.) to excessive nitrogen and phosphorus application. Journal of Agricultural Science and Technology 15:479−89

    Google Scholar

    [68]

    Bolinder MA, Janzen HH, Gregorich EG, Angers DA, VandenBygaart AJ. 2007. An approach for estimating net primary productivity and annual carbon inputs to soil for common agricultural crops in Canada. Agriculture, Ecosystems & Environment 118:29−42

    doi: 10.1016/j.agee.2006.05.013

    CrossRef   Google Scholar

    [69]

    Amanullah. 2017. Integrated use of organic carbon, plant nutrients and bio-fertilizers is key to improve field crops productivity under arid and semiarid climates. FAO (2017) Proceedings of the Global Symposium on Soil Organic Carbon, Rome, Italy, 21−23 March 2017. Rome: Food and Agriculture Organization of the United Nations. pp: 480−81.

    [70]

    Amanullah, Fahad S. 2018. Integrated nutrient management in corn production: Symbiosis for food security and grower's income in arid and semiarid climates. In Corn - Production and Human Health in Changing Climate, eds. Amanullah, Fahad S. London, UK: InTech. pp. 3−12. https://doi.org/0.5772/intechopen.80995

    [71]

    Lal R. 2006. Enhancing crop yields in the developing countries through restoration of the soil organic carbon pool in agricultural lands. Land Degradation & Development 17:197−209

    doi: 10.1002/ldr.696

    CrossRef   Google Scholar

    [72]

    Zengeni R, Chaplot V, Shimelis H, Mathew I, Mbava N, et al. 2021. Water use efficiency and carbon sequestration potential of indigenous crops. Water Research Commission (WRC), School of Agricultural, Earth and Environmental Sciences University of KwaZulu-Natal

    [73]

    McKendry P. 2002. Energy production from biomass (part 1): overview of biomass. Bioresource Technology 83:37−46

    doi: 10.1016/s0960-8524(01)00118-3

    CrossRef   Google Scholar

    [74]

    Amanullah, Khalid S. 2020. Agronomy - food security - climate change and the sustainable development goals. In Agronomy – Climate Change & Food Security, ed. Amanullah. UK: Intech Open. https://doi.org/10.5772/intechopen.92690

  • Cite this article

    Amanullah. 2023. A simple model for estimation of above and below ground carbon in cereal crops. Technology in Agronomy 3:8 doi: 10.48130/TIA-2023-0008
    Amanullah. 2023. A simple model for estimation of above and below ground carbon in cereal crops. Technology in Agronomy 3:8 doi: 10.48130/TIA-2023-0008

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A simple model for estimation of above and below ground carbon in cereal crops

Technology in Agronomy  3 Article number: 8  (2023)  |  Cite this article

Abstract: Carbon (C) is an essential part of healthy soil. Healthy soils play an important role in improving the life of all living organisms on earth (plants, humans, animals, birds, insects, microbes etc.). Best agronomic practices for field crop production sequester more carbon (due to higher photosynthesis) below and above the ground that makes the soils healthy and sustainable. Healthy soils increase yield per unit area and so reduce the problem of food insecurity. Higher photosynthetic efficiency (higher CO2 uptake by the plants) reduces the problem of global warming and climate change. According to an estimate, plants capture about 860 gigatons of CO2 each year from the atmosphere, storing it in their shoots, and roots (1 kg of carbon is equal to 3.67 kg of CO2). The aim of this study was to develop a simple calculation (model) for researchers to easily estimate the carbon content (CC) capture by plants in below (roots) and above ground (shoots) parts. Considerable variation in total CC (TCC) accumulation and its partitioning into above ground parts (ACC) and below ground parts (BCC) exists which depends on crop species and genotypes, crop nutrition, crop competitions and intercropping, fertilizers application, irrigation, tillage, biotic and abiotic stresses, soil types and environment etc. The CC estimation is explained in detail with four examples on major cereal crops (wheat, rice, maize and barley) for the world leading countries in 2018−2019. In the first example using wheat, the TCC estimated for wheat crop in Pakistan was 37.4 metric tons (MT) of which 30.5 MT was allocated into ACC (shoots) and 6.9 MT into BCC (roots). The highest value of TCC accumulation for wheat crop was estimated for the European Union which was 216.3 MT (176.4 ACC + 39.9 BCC). In the second example using rice crop, TCC for the world leading countries was estimated and the leading country was China with TCC of 161.7 MT (131.9 ACC + 29.8 BCC). Example three is about the CC estimation for maize crop, and the leading country was USA having the highest TCC value of 505.3 MT (ACC = 412.1 MT, BCC = 93.2 MT). The Russian Federation ranked first for barley crop and the highest TCC value of 29.2 MT was recorded (23.8 MT ACC + 5.4 MT BCC). It was confirmed while using this model that out of the 100% (TCC) fixed, about 82% CC is partitioned into above ground parts (ACC) and the remaining 18% CC is allocated into below ground parts (BCC). Due to this model, we can easily calculate the TCC accumulation and its partitioning into ACC and BCC per unit area (kg·ha−1). For example, the TCC was easily calculated for the 40 world leading countries for wheat, rice, maize and barley during 2019. The results revealed that the TCC ranged from 4,414 to 13,243 kg·ha−1 for wheat, 4,578 to 11,444 kg·ha−1 for rice, 5,150 to 15,450 kg·ha1 for maize, and 3,443 to 13,733 kg·ha−1 for barley among the top 40 countries. This is the most simplified approach for estimating carbon content in the below-ground (roots) and above-ground (shoots) parts of field crops.

    • Crop growth and yield depends on the fixed carbon content (CC) and their distribution to plant parts (e.g. roots and shoots). Understanding and calculating the total CC (TCC) accumulated in field crops is very important due to the current issues of food security and global warming. However, there is a lack of research that shows how much CC is partitioned into the roots and shoots. Our previous research work confirmed that the increase in CC in plant tissues (roots and shoots) depends on total dry matter accumulation and partitioning[14 ], because plant growth and yield correlates with net carbon gain on a whole plant basis[5, 6 ].

      The IPCC report[7] revealed that about 1.2 billion tonnes of carbon at annual rate of 4‰ could be stocked every year for the sustainability of agricultural systems. As the crop growth and yield depends on the total CC (TCC) of plants, therefore, any agronomic practices that help the plants to sequester more atmospheric CO2 (photosynthesis) increases the TCC accumulation in plants in its distribution to below ground CC to roots (BCC) and above ground CC to shoots (ACC). Therefore, crop production may be defined as: maximizing photosynthetic efficiency of crops to store more carbon above (ACC) and below (BCC) ground parts. The increase in CC above ground part (ACC) depends on: number and size of leaves, number of tillers, reproductive tillers, stems, seed size and number, grain yield and harvest index etc., increase partitioning of CC for better roots development depends on: roots number and length, root proliferation and total root biomass. The increase in CC of roots (BCC) will help the plants to uptake more water and nutrients from the soil and transfers it for better shoot development (ACC) e.g. increase in grain yield, yield components and harvest index.

      The TCC accumulation and its partitioning in plant bodies depends on three major factors: (1) plant genotypes e.g. plant species, varieties, hybrids, exhaustive (grasses) and restorative (legumes) crops, growth habit, growth stages, photosynthesis, C4 crops (e.g. maize, sorghum, millets, etc.) and C3 crops (e.g. wheat, rice, and barley etc.); (2) agronomic practices (chemical fertilizers, organic fertilizers, biofertilizers, plant nutrition, irrigation, tillage practices, soil types, SOC, plant density, seed rates, sowing time, etc. ); and (3) environmental condition viz. biotic stresses (plant competition, weeds, diseases, insects, pests, etc.) and abiotic stresses (low and high temperature stress, low and high water stress, light quality and duration, wind, chemicals, gases, soil pollution, water pollution, etc.).

      In recent years, many international organizations[818] and researchers[1943] reported about the importance of carbon footprints in plants, animals, soil, water, environment, ecosystems etc. There is still a lack of comprehensive research and reports on the precise amount of carbon sequestered or stored by individual plants. Because carbon estimation in field crops, especially in roots, is very difficult, costly and time consuming.

      The primary objective of this paper is to create a simplified model for estimating the allocation of above-ground carbon content (ACC) and below-ground carbon content (BCC) in field crops, specifically cereals. The purpose of developing a simplified model is to facilitate the estimation of carbon content partitioning in field crops, such as winter crops (e.g., wheat and barley) and summer crops (e.g., maize and rice), specifically targeting students and researchers. This model aims to simplify the process and make it more accessible for those interested in studying carbon content allocation in field crops.

    • For the estimation of the total carbon content (TCC) accumulated by plants and its distribution (partitioning) into above ground (shoots) and below ground (roots) parts, efforts were made to calculate the two important factors for above ground parts (ACC) and below ground parts (BCC), 0.42 (% CC in shoot biomass) and 0.38 (% CC in root biomass), respectively. Then three simple equations (1, 2 and 3) were developed to easily estimate the CC in above ground biomass (AGB), below ground biomass (BGB) and total biomass (TBM):

      $ ACC = AGB \times 0.42 $ (1)
      $ BCC = BGB \times 0.38 $ (2)
      $ TCC = ACC + BCC $ (3)

      The total CC (TCC) per plant or per unit area can be easily calculated in field crops by just adding ACC with BCC as shown in Eqn (3).

      Based on the model developed in this study: Out of the 100% total carbon content (TCC) fixed/accumulated by field crops, 82% is partitioned into shoots or above ground carbon content (ACC) and 18% into roots or below ground carbon content (BCC). On the other hand, out of the 100% total biomass (shoots biomass + roots biomass on dry basis) (TBM) accumulation by field crops, 80% is partitioned into above ground biomass (AGB) and 20% into below ground biomass (BGB).

      Note: Multiplying the amount of CO2 by 12/44 or 0.27 is equal to the amount of carbon, means that 1 kg of CO2 is equal to 0.27 kg of carbon. On other hand, multiplying the amount of carbon by 44/12 or 3.67 (44/12) is equal to the amount of CO2, means that 1 kg of carbon is equal to 3.67 kg of CO2 (where 12 is the molecular weight of carbon, and 44 is the molecular weight of CO2 (C + O2 = 12 + 16 × 2 = 44).

    • In 2018, wheat produced in metric tonnes (MT) and the total carbon content (TCC) accumulated and partitioned into roots or below ground CC (BCC) and shoots, or above ground CC (ACC) for the world leading countries was calculated through this model (Table 1). For example, in 2018, the total wheat produced in Pakistan was 25.4 MT[2, 44].

      Table 1.  Approximate estimation of carbon content (CC) fixed by wheat crop in metric tons (MT) for the leading countries in the world during 2018−2019.

      CountriesMetric tons (MT)
      GYAGBACCBGBBCCTBMTCC
      European Union147.0420.0176.4105.039.9525.0216.3
      China (mainland)126.7362.0152.090.534.4452.5186.4
      India98.6281.7118.370.426.8352.1145.1
      Russian Federation72.0205.786.451.419.5257.1105.9
      United States of America49.7142.059.635.513.5177.573.1
      Canada31.389.437.622.48.5111.846.1
      Pakistan25.472.630.518.16.990.737.4
      Ukraine23.466.928.116.76.483.634.4
      Australia21.962.626.315.65.978.232.2
      Turkey21.060.025.215.05.775.030.9
      Argentina20.057.124.014.35.471.429.4
      Kazakhstan14.040.016.810.03.850.020.6
      Iran Islamic Rep. 13.438.316.19.63.647.919.7
      Other countries71.7204.986.051.219.5256.1105.5
      World736.12103.1883.3525.8199.82628.91083.1
      Source: FAO outlook[11] and Amanullah et al.[64]. Where: CC = Carbon content, MT = Metric tons, GY = Grain yield, AGB = Above ground biomass, ACC = Above ground CC, BGB = Below ground biomass, BCC = Below ground CC, TBM = Total biomass (AGB + BGB), TCC = Total CC (ACC + BCC).

      The above ground biomass (AGB) or shoot dry weight (shoot biomass) was calculated using Eqn 4:

      $ \begin{split}{\boldsymbol{AGB}} =\;&{\boldsymbol{ Grain}}\; {\boldsymbol{Production}}\; {\bf\div}{\bf{ 0.35}} ({\boldsymbol{Factor}}) \\=\;& 25.4 \div 0.35 \\=\;& 72.6 \;(MT)\end{split} $ (4)

      The carbon content of the AGB or shoot CC (ACC) was calculated using the following equation:

      $\begin{split} {\boldsymbol{ACC}} =\;&{\boldsymbol{ AGB}} \times {\boldsymbol{factor}}\; ({\bf{0.42}})\\ =\;& 72.6 \times 0.42 \\=\;& 30.5 MT \;({\bf{82}}{ {\%}})\end{split}\tag{1} $

      The total biomass (TBM) (shoots + roots) was calculated using Eqn 5:

      $\begin{split} {\boldsymbol{TBM}} =\;&{\boldsymbol{ AGB}} \times {\bf{1.25}} \;({\boldsymbol{Factor}})\\ =\;& {\bf{72.6}} {\bf\times}{\bf{ 1.25}}\\ =\;&{\bf{ 90.7}}{\boldsymbol{ MT}}\end{split} $ (5)

      The below ground biomass (BGB) or root biomass was calculated using Eqn 6:

      $\begin{split}{\boldsymbol{ BGB}} =\;&{\boldsymbol{ TBM}}{\bf \times} {\bf{0.20}}\; ({\boldsymbol{Factor}})\\ =\;& 90.7 \times 0.20 \\=\;& 18.1 MT \end{split}$ (6)

      The CC of the BGB or root biomass (BCC) was calculated using Eqn 2:

      $ \begin{split}{\boldsymbol{BCC}} =\;&{\boldsymbol{ BGB}} {\bf\times} {\boldsymbol{factor}}\; ({\bf{0.38}}) \\=\;& 18.1 \times 0.38\\ =\;& 6.9 MT\; ({\bf{18}}{ {\%}})\end{split} \tag{2}$

      The total CC (TCC) fixed by wheat in Pakistan during 2018 was calculated using Eqn 3:

      $\begin{split}{\boldsymbol{ TCC}} = \;&{\boldsymbol{ACC}} + {\boldsymbol{BCC}}\\ =\;&\bf 30.5 \;(82{ {\%}}) + 6.9 \;(18{ {\%}}) \\=\;&{\bf{ 37.4}}{\boldsymbol{ MT}}\; (\bf100{ {\%}})\end{split}\tag{3} $
    • In 2018, rice produced in metric tonnes (MT) and the total carbon content (CC) fixed in rice below (BCC) and above (ACC) ground parts for the world leading countries was calculated (Table 2). For example, in 2018 the total rice produced in China was 141.3 MT[2, 44].

      Table 2.  Approximate estimation of carbon content (CC) fixed by rice crop in metric tons (MT) for the leading countries in the world during 2018.

      CountriesMetric tons (MT)
      GYAGBACCBGBBCCTBMTCC
      China (mainland)141.3314.0131.978.529.8392.5161.7
      India113.5252.2105.963.124.0315.3129.9
      Indonesia46.7103.843.625.99.9129.753.4
      Bangladesh35.378.432.919.67.598.140.4
      Viet Nam28.763.826.815.96.179.732.8
      Thailand22.850.721.312.74.863.326.1
      Myanmar18.240.417.010.13.850.620.8
      Philippines12.928.712.07.22.735.814.8
      Brazil817.87.54.41.722.29.2
      Japan7.516.77.04.21.620.88.6
      Pakistan7.616.97.14.21.621.18.7
      United States of America6.514.46.13.61.418.17.4
      Cambodia6.414.26.03.61.417.87.3
      Egypt4.29.33.92.30.911.74.8
      Nigeria4.39.64.02.40.911.94.9
      World511.41136.4477.3284.1108.01420.6585.3
      Source: FAO outlook [11] and Amanullah et al.[64]. Where: CC = Carbon content, MT = Metric tons, GY = Grain yield, AGB = Above ground biomass, ACC = Above ground CC, BGB = Below ground biomass, BCC = Below ground CC, TBM = Total biomass (AGB + BGB), TCC = Total CC (ACC + BCC).

      The above ground biomass (AGB) or shoots dry weight (shoot biomass) was calculated using Eqn 4:

      $\begin{split}{\boldsymbol{ AGB}} =\;&{\boldsymbol{ Grain}}\; {\boldsymbol{Production}} \bf\div 0.45\; ({\boldsymbol{Factor}}) \\=\;& 141.3 \div 0.45\\ =\;& 314.0\; (MT)\end{split}\tag{4} $

      The carbon content of the AGB or shoots (ACC) was calculated using the following Eqn 1:

      $\begin{split}{\boldsymbol{ ACC}} =\;&{\boldsymbol{ AGB}} {\bf\times} {\boldsymbol{factor}}\; ({\bf{0.42}}) \\=\;& 314.0 \times 0.42 \\=\;& 131.9 MT\; (82{\text{%}})\end{split}\tag{1} $

      The total biomass (TBM) (shoots + roots) was calculated using Eqn 5:

      $\begin{split}{\boldsymbol{ TBM}} = \;&{\boldsymbol{AGB}} {\bf\times}{\bf{ 1.25}} \\=\;&\bf 314 \times 1.25\\ =\;&{\bf {392.5}} {\boldsymbol{MT}}\end{split}\tag{5} $

      The below ground biomass (BGB) or root biomass was calculated using Eqn 6:

      $ \begin{split}{\boldsymbol{BGB}} =\;&{\boldsymbol{ TBM}} {\bf\times} {\bf{0.20}}\; ({\boldsymbol{Factor}})\\ =\;& 392.5 \times 0.20 \\=\;& 78.5\; MT\end{split}\tag{6} $

      The CC of the BGB or root biomass (BCC) was calculated using Eqn 2:

      $\begin{split}{\boldsymbol{ BCC}} =\;&{\boldsymbol{ BGB}} {\bf\times} {\boldsymbol{factor}}\; ({\bf{0.38}})\\ =\;& 78.5 \times 0.38 \\=\;& 29.8\; MT\; ({\bf{18}}{ {\%}})\end{split}\tag{2} $

      The total CC (TCC) fixed by rice crop in china during 2018 was calculated using Eqn 3:

      $\begin{split}{\boldsymbol{ TCC}} =\;&{\boldsymbol{ ACC}} + {\boldsymbol{BCC}}\\ =\;&{\bf{ 131.9}}\; ({\bf{82}}{ {\%}}) + {\bf{29.8}}\; ({\bf{18}}{ {\%}})\\ =\;&{\bf {161.7}}\;{\boldsymbol{ MT}}\; ({\bf{100}}{ {\%}})\end{split}\tag{3} $
    • In 2018, maize produced in metric tonnes (MT) and the TCC, BCC and ACC for maize in world leading countries was calculated (Table 3). For example, in 2018 the total maize produced in USA was 392.5 MT[2, 44].

      Table 3.  Approximate estimation of carbon content (CC) fixed by maize crop in metric tons (MT) for the leading countries in the world during 2018.

      CountriesMetric tons (MT)
      GYAGBACCBGBBCCTBMTCC
      United States of America392.5981.1412.1245.393.21226.4505.3
      China (mainland)257.2642.9270.0160.761.1803.7331.1
      Brazil82.3205.786.451.419.5257.2105.9
      Argentina43.5108.745.627.210.3135.856.0
      Ukraine35.889.537.622.48.5111.946.1
      Indonesia30.375.631.818.97.294.539.0
      India27.869.629.217.46.686.935.8
      Mexico27.267.928.517.06.584.935.0
      Romania18.746.719.611.74.458.324.0
      Canada13.934.714.68.73.343.417.9
      France12.731.713.37.93.039.616.3
      South Africa12.531.313.17.83.039.116.1
      Russian Federation11.428.512.07.12.735.714.7
      Nigeria10.225.410.76.32.431.713.1
      Hungary8.019.98.45.01.924.910.3
      Philippines7.819.48.24.91.824.310.0
      Ethiopia7.418.47.74.61.723.09.5
      Egypt7.318.37.74.61.722.89.4
      Serbia7.017.47.34.41.721.89.0
      Pakistan6.315.86.63.91.519.78.1
      World
      Source: FAO outlook [11] (Accessed on 5-5-2020). Where: CC = Carbon content, MT = Metric tons, GY = Grain yield, AGB = Above ground biomass, ACC = Above ground CC, BGB = Below ground biomass, BCC = Below ground CC, TBM = Total biomass (AGB + BGB), TCC = Total CC (ACC + BCC).

      The above ground biomass (AGB) or shoot biomass was calculated using Eqn 4:

      $ \begin{split}{\boldsymbol{AGB}} =\;&{\boldsymbol{ Grain}}\; {\boldsymbol{Production}} {\bf\div} {\bf{0.40}}\; ({\boldsymbol{Factor}}) \\=\;& 392.5 \div 0.40\\ =\;& 981.1\; (MT)\end{split}\tag{4} $

      The carbon content of the AGB or shoot CC (ACC) was calculated using the following Eqn 1:

      $\begin{split}{\boldsymbol{ ACC}} =\;&{\boldsymbol{ AGB}} {\bf\times} {\boldsymbol{factor}}\; ({\bf{0.42}}) \\=\;& 981.1 \times 0.42 \\=\;& 412.1 \;MT\; ({\bf{82}}{ {\%}})\end{split} \tag{1}$

      The total biomass (TBM) (shoots + roots dry weights) was calculated using Eqn 5:

      $\begin{split}{\boldsymbol{ TBM}} =\;& {\boldsymbol{AGB}} {\bf\times} {\bf{1.25}}\\ =\;&{\bf{ 981.1}} {\bf\times} {\bf{1.25}} \\=\;&{\bf{ 1226.4}}\;{\boldsymbol{ MT}}\end{split}\tag{5} $

      The below ground biomass (BGB) or root dry weight (root biomass) was calculated using equation-6:

      $\begin{split}{\boldsymbol{ BGB}} =\;&{\boldsymbol{ TBM}} {\bf\times} {\bf{0.20}}\; ({\boldsymbol{Factor}})\\ =\;& 1226.4 \times 0.20 \\=\;& 245.3\; MT\end{split}\tag{6} $

      The CC of the BGB or root biomass (BCC) was calculated using Eqn 2:

      $\begin{split} {\boldsymbol{BCC}} =\;&{\boldsymbol{ BGB}} {\bf\times} {\boldsymbol{factor}}\; ({\bf{0.38}}) \\=\;& 245.3 \times 0.38 \\=\;& 93.2 \;MT\; ({\bf{18}}{ {\%}})\end{split}\tag{2} $

      The total CC (TCC) accumulated by maize crop in the United States of America (USA) during 2018 was calculated using Eqn 3:

      $\begin{split}{\boldsymbol{ TCC}} =\;&{\boldsymbol{ ACC}} + {\boldsymbol{BCC}}\\ =\;&{\bf{ 412.1}}\; ({\bf{82}}{ {\%}}) + {\bf{93.2}}\; ({\bf{18}}{ {\%}})\\ =\;&{\bf{ 505.3}}\;{\boldsymbol{ MT}}\; ({\bf{100}}{ {\%}})\end{split}\tag{3} $
    • In 2018, barley produced in MT and the TCC fixed in the barley growing area in the world leading countries was estimated (Table 4). For example, in 2018 the total barley produced in the Russian Federation was 17.0 MT[2, 44].

      Table 4.  Approximate estimation of carbon content (CC) fixed by barley crop in metric tons (MT) for the leading countries in the world during 2018−2019.

      CountriesMetric tons (MT)
      GYAGBACCBGBBCCTBMTCC
      Russian Federation17.056.623.814.25.470.829.2
      France11.237.315.79.33.546.619.2
      Germany9.631.913.48.03.039.916.5
      Australia9.330.813.07.72.938.615.9
      Spain9.130.412.87.62.938.015.7
      Canada8.427.911.77.02.734.914.4
      Ukraine7.324.510.36.12.330.612.6
      Turkey7.023.39.85.82.229.212.0
      United Kingdom6.521.79.15.42.127.111.2
      Argentina5.116.97.14.21.621.18.7
      Kazakhstan4.013.25.63.31.316.56.8
      Denmark3.511.64.92.91.114.56.0
      United States of America3.311.14.72.81.113.95.7
      Poland3.010.24.32.51.012.75.2
      Morocco2.99.54.02.40.911.94.9
      Iran2.89.33.92.30.911.74.8
      Ethiopia2.17.02.91.80.78.83.6
      Algeria2.06.52.71.60.68.23.4
      Romania1.96.22.61.60.67.83.2
      India1.85.92.51.50.67.43.1
      World
      Source: FAO outlook[11] (Accessed on 5-5-2020). Where: CC = Carbon content, MT = Metric tons, GY = Grain yield, AGB = Above ground biomass, ACC = Above ground CC, BGB = Below ground biomass, BCC = Below ground CC, TBM = Total biomass (AGB + BGB), TCC = Total CC (ACC + BCC).

      The above ground biomass (AGB) or shoot biomass was calculated using Eqn 4:

      $\begin{split} {\boldsymbol{AGB}} =\;&{\boldsymbol{ Grain}} \;{\boldsymbol{Production}} {\bf\div} {\bf{0.30}}\; ({\boldsymbol{Factor}}) \\=\;& 17.0 \div 0.30 \\=\;& 56.6\; (MT)\end{split} \tag{4}$

      The carbon content of the AGB or shoot CC (ACC) was calculated using the following Eqn 1:

      $\begin{split}{\boldsymbol{ ACC}} =\;&{\boldsymbol{ AGB}} {\bf\times} {\boldsymbol{factor}}\; ({\bf{0.42}})\\ =\;& 56.6 \times 0.42 \\=\;& 23.8\; MT\; ({\bf{82}}{ {\%}})\end{split}\tag{1} $

      The total biomass (TBM) (shoots + roots dry weights) was calculated using Eqn 5:

      $\begin{split} {\boldsymbol{TBM}} =\;&{\boldsymbol{ AGB}} {\bf\times} {\bf{1.25}}\\ =\;&{\bf{ 56.6}} {\bf\times} {\bf{1.25}}\\ =\;&{\bf{ 70.8}}\;{\boldsymbol{ MT}}\end{split}\tag{5} $

      The below ground biomass (BGB) or root dry weight (root biomass) was calculated using Eqn 6:

      $\begin{split}{\boldsymbol{ BGB}} =\;&{\boldsymbol{ TBM}} {\bf\times} {\bf{0.20}}\; ({\boldsymbol{Factor}})\\ =\;& 70.8 \times 0.20 \\=\;& 14.2\; MT\end{split}\tag{6} $

      The CC of the BGB or root biomass (BCC) was calculated using Eqn 2:

      $ \begin{split}{\boldsymbol{BCC}} =\;&{\boldsymbol{ BGB}} {\bf\times} {\boldsymbol{factor}}\; ({\bf{0.38}})\\ =\;& 14.2 \times 0.38\\ =\;& 5.4\; MT\; ({\bf{18}}{ {\%}})\end{split}\tag{2} $

      The total CC (TCC) fixed by wheat in Pakistan during 2018 was calculated using Eqn 3:

      $\begin{split}{\boldsymbol{ TCC}} =\;&{\boldsymbol{ ACC}} +{\boldsymbol{ BCC}}\\ =\;&{\bf{ 23.8}}\; ({\bf{82}}{ {\%}}) + {\bf{5.4}} \;({\bf{18}}{ {\%}})\\ =\;& {\bf{29.2}}\;{\boldsymbol{ MT}}\; ({\bf{100}}{ {\%}})\end{split}\tag{3} $

      The TCC (shoots + roots), ACC (shoots) and BCC (roots) for cereal crops can be easily calculated:

      ParameterEqual toParameterSymbolFactorEquation
      ACC=AGB×0.421
      BCC=BGB×0.382
      TCC=ACC+BCC3
      AGB=GY÷0.35*4
      TBM=AGB×1.255
      BGB=TBM×0.206
      TBM=AGB+BGB7
      Where: W, R, M and B stands for wheat, rice, maize and barley, respectively. Factor: * 0.35 for wheat, 0.45 for rice, 0.40 for maize, and 0.30 for barley.
      GY = Grain yield; AGB = Above ground biomass; ACC = Above ground CC; BGB = Below ground biomass; BCC = Below ground CC; TBM = Total biomass (AGB + BGB); TCC = Total CC (ACC + BCC).
    • This model was used to calculate the TCC (kg·ha−1) accumulated by the four major cereal crops (wheat, rice, maize and barley) and its distribution into ACC (kg·ha−1) and BCC (kg·ha−1) for the 40 leading countries during 2019 (USDA). The grain yield data (t ha−1) was accessed on the USDA website on 8th May 2020 and converted into kg·ha1 (t·ha−1 × 1,000 = kg·ha−1). The results revealed that remarkable variations were observed in TCC, ACC and BCC among the 40 countries for each crop. For example, the TCC for wheat crop ranged from 4,414 for Pakistan to 13,243 kg·ha−1 for New Zealand (Table 5). For the rice crop, the TCC ranged from 4578 (Philippines) to 11,444 kg·ha−1 (Australia) as shown in Table 6. The lowest TCC (5,150 kg·ha−1) in the case of maize crop was calculated for Korea Democratic and the highest (15,450 kg·ha−1) for Chile (Table 7). In the case of barley, the TCC ranged from 3,443 (Algeria) to 13,733 kg·ha−1 (Chile), respectively (Table 8). These results revealed that out of the TCC (100%) accumulated by the crops (wheat, rice, maize and barley), 82% was partitioned into ACC (shoots) and 18% to BCC (roots). The higher TCC partitioning into shoots (ACC) than roots (BCC) in different crop species was the possible cause of higher shoot dry matter (shoot biomass) than total root dry matter (roots biomass) production[4547]. The differences in the ACC and BCC among the four crop species was attributed to the genetic differences among the crops species[4, 46,47]. Variation in C content among plant organs are also reported in previous research[48,49].

      Table 5.  Carbon content (kg·ha−1) calculation for wheat crop in 40 leading countries in the world during 2019−2020.

      CountriesKilograms per hectare (kg·ha−1)
      GYACCBCCTCC
      New Zealand900010800244313243
      Namibia6000720016298829
      Saudi Arabia6000720016298829
      Switzerland6000720016298829
      Chile6000720016298829
      China6000720016298829
      EU-276000720016298829
      Egypt6000720016298829
      Zambia6000720016298829
      Uzbekistan5000600013577357
      Japan5000600013577357
      Mexico5000600013577357
      Norway5000600013577357
      Macedonia4000480010865886
      Mali4000480010865886
      Serbia4000480010865886
      Ukraine4000480010865886
      Korea, Republic4000480010865886
      Belarus4000480010865886
      Albania4000480010865886
      Bosnia-Herzegovina4000480010865886
      Bangladesh4000480010865886
      Zimbabwe4000480010865886
      South Africa300036008144414
      Azerbaijan300036008144414
      Armenia300036008144414
      Argentina300036008144414
      Canada300036008144414
      Brazil300036008144414
      Iran300036008144414
      India300036008144414
      United States of America300036008144414
      Uruguay300036008144414
      Tajikistan300036008144414
      Turkey300036008144414
      Russian Federation300036008144414
      Pakistan300036008144414
      Sudan300036008144414
      Syrian Arab Rep.300036008144414
      Lebanon300036008144414
      Grain yield data of 2019 taken from USDA website accessed on 8 May 2020. *GY (grain yield), CC (carbon content), ACC (above ground CC), BCC (below ground CC) and TCC (total below and above ground CC).

      Table 6.  Carbon content (kg·ha−1) calculation for rice crop in 40 leading countries in the world during 2019.

      CountriesKilograms per hectare (kg ha−1)
      GYACCBCCTCC
      Australia100009333211111444
      Turkey90008400190010300
      Peru8000746716899156
      Morocco8000746716899156
      Egypt8000746716899156
      United States of America8000746716899156
      Uruguay8000746716899156
      EU-277000653314788011
      Japan7000653314788011
      Argentina7000653314788011
      Chile7000653314788011
      China7000653314788011
      Korea7000653314788011
      Mexico6000560012676867
      Paraguay6000560012676867
      Russian Federation6000560012676867
      El Salvador6000560012676867
      Taiwan6000560012676867
      Brazil6000560012676867
      Guyana6000560012676867
      Viet Nam6000560012676867
      Ukraine5000466710565722
      Indonesia5000466710565722
      Iraq5000466710565722
      Iran5000466710565722
      Dominican Republic5000466710565722
      Bangladesh5000466710565722
      Colombia5000466710565722
      Suriname5000466710565722
      Mauritania5000466710565722
      Niger5000466710565722
      Kazakhstan5000466710565722
      Sri Lanka400037338444578
      Nicaragua400037338444578
      Nepal400037338444578
      Panama400037338444578
      Korea, Democratic400037338444578
      Malaysia400037338444578
      Senegal400037338444578
      Philippines400037338444578
      Grain yield data of 2019 taken from USDA website accessed on 8 May 2020. * GY (grain yield), CC (carbon content), ACC (above ground CC), BCC (below ground CC) and TCC (total below and above ground CC).

      Table 7.  Carbon content (kg·ha−1) calculation for maize crop in 40 leading countries in the world during 2019.

      CountriesKilograms per hectare (kg·ha−1)
      GYACCBCCTCC
      Chile1200012600285015450
      Turkey1200012600285015450
      United States1100011550261314163
      New Zealand1100011550261314163
      Uzbekistan1000010500237512875
      Jordan1000010500237512875
      Switzerland90009450213811588
      Canada90009450213811588
      Argentina80008400190010300
      Bangladesh80008400190010300
      Egypt80008400190010300
      EU-277000735016639013
      Albania7000735016639013
      Australia7000735016639013
      Iran7000735016639013
      Kyrgyzstan7000735016639013
      Uruguay7000735016639013
      Ukraine7000735016639013
      Serbia7000735016639013
      Russian Federation6000630014257725
      Saudi Arabia6000630014257725
      Paraguay6000630014257725
      Taiwan6000630014257725
      Tajikistan6000630014257725
      Iraq6000630014257725
      Kazakhstan6000630014257725
      Lao6000630014257725
      Malaysia6000630014257725
      Azerbaijan6000630014257725
      Bosnia-Herzegovina6000630014257725
      Brazil6000630014257725
      Belarus6000630014257725
      China6000630014257725
      Korea, Republic5000525011886438
      Cambodia5000525011886438
      Viet Nam5000525011886438
      South Africa5000525011886438
      Pakistan5000525011886438
      Thailand400042009505150
      Korea, Democratic400042009505150
      Grain yield data of 2019 taken from USDA website accessed on 8 May 2020. * GY (grain yield), CC (carbon content), ACC (above ground CC), BCC (below ground CC) and TCC (total below and above ground CC).

      Table 8.  Carbon content (kg·ha−1) calculation for barley crop in 40 leading countries in the world during 2019−2020.

      CountriesKilograms per hectare (kg·ha−1)
      GYACCBCCTCC
      Chile800011200253313733
      New Zealand70009800221712017
      Zimbabwe60008400190010300
      Switzerland60008400190010300
      EU-275000700015838583
      Saudi Arabia5000700015838583
      Ukraine4000560012676867
      United States4000560012676867
      Uruguay4000560012676867
      Serbia4000560012676867
      Norway4000560012676867
      Korea, Republic4000560012676867
      Brazil4000560012676867
      Belarus4000560012676867
      Canada4000560012676867
      Argentina4000560012676867
      Azerbaijan300042009505150
      Bosnia- Herzegovina300042009505150
      China300042009505150
      Japan300042009505150
      Kenya300042009505150
      India300042009505150
      Mexico300042009505150
      South Africa300042009505150
      Tunisia200028006333433
      Turkey200028006333433
      Ethiopia200028006333433
      Russian Federation200028006333433
      Peru200028006333433
      Uzbekistan200028006333433
      Tajikistan200028006333433
      Iran200028006333433
      Georgia200028006333433
      Kyrgyzstan200028006333433
      Lebanon200028006333433
      Moldova200028006333433
      Macedonia200028006333433
      Colombia200028006333433
      Algeria200028006333433
      Grain yield data of 2019 taken from USDA website accessed on 8 May 2020. * GY (grain yield), CC (carbon content), ACC (above ground CC), BCC (below ground CC) and TCC (total below and above ground CC).

      The TCC accumulation in crop plants and its partitioning into above ground parts (ACC) and below ground parts (BCC) depends on these three major factors: (1) plant genotypes (species, varieties, hybrids, growth habit, growth stages); (2) agronomic practices (chemical fertilizers, organic fertilizers, biofertilizers, plant nutrition, irrigation, tillage practices, soil types, SOC, plant density, seed rates, sowing time, etc. ); and (3) environmental condition viz. biotic stresses (plant competition, weeds, diseases, insects, pests, etc.) and abiotic stresses (low and high temperature stress, low and high water stress, light quality and duration, wind, chemicals, gases, soil pollution, water pollution etc.). Total dry matter accumulation and its partitioning into roots and shoots depends on plant nutrition[46, 49], light availability[50], soil types[45], plant competitions[51], organic sources[52], beneficial microbes[52,53], plant species[4, 45,54], plants genotypes[2, 55], plant tissues[48, 5658], and plant growth stages[46, 59,60], etc.

      The differences in the TCC accumulation and its partitioning into ACC and BCC in different crop species under study may be attributed to the differences in genetic makeup and differences in plant heights, leaf area, leaf area index and crop growth rate, water and nutrients use efficiency[45,46, 61]. Bagrintseva & Nosov[62] and Mut et al.[63] reported changes in the total biomass accumulation in different crops. Therefore, crops which could sequester more carbon above (shoots) and below ground (roots) indicating more carbon dioxide sequestration from the atmosphere and therefore the cultivation of these crops could help reduce global warming. Therefore, plant breeder's efforts to produce crop species and ideotypes with higher TCC accumulation could be useful. As the cereals and grasses are executive crops[64], so the use of sustainable soil management practices[8, 11, 65], could also increase the TCC accumulation and reduce CO2 in the atmosphere.

      In our previous experiments[45, 66], the NPK source which was associated with higher total biomass (TCC) also increases both root biomass (BCC) and shoot biomass (ACC). The increase and decrease in the CC accumulation in both roots (BCC) and shoots (ACC) in this study showed positive relationship with increase in biomass production and partitioning[1] and better growth[45,46]. Bagrintseva & Nosov[62] reported more DM partitioning in wheat and barley with combined application of N + P + K than N + P. Amanullah & Stewart[67 ] reported that N toxicity had reduced total biomass formation and partitioning into shoots (ACC) and roots (BCC).

      In other studies[59] where both organic and inorganic soils were compared. The results revealed that the higher BCC under three organic soils (S3, S4 and S5) at different growth stages was attributed to the longer root lengths and formation of a greater number of roots per plant[59], that increased water use efficiency that allocated more total biomass (TCC) into below ground biomass (BCC)[45,46]. In contrast, the lesser BCC obtained under inorganic soils (S1 and S2) was attributed the shorter root lengths and less number of roots per plant produced[59], and low WUE with lesser allocation of dry matter into roots[45]. Likewise, the higher ACC under three organic soils (S3, S4 and S5) at different growth stages was attributed to formation of taller plants with more number of leaves and larger leaf area, and formation of a greater number of tillers per plant[59] and high WUE with greater allocation of dry matter into shoots[45]. In contrast, the lesser ACC obtained under inorganic soils (S1 and S2) was attributed to development of shorter plants with less number of leaves and less leaf area and formation of a less number of tillers per plant[59] and low WUE with and so lesser allocation of DM into shoots[45].

      Integrated nutrients management in field crop production, especially plant residue incorporation improve soil fertility that improves crop growth and total biomass[24, 68] and reduces the problem of food security. Amanullah,[69] in a FAO global conference (Rome, Italy) reported that integrated use of organic carbon source (animal manures and plant residues), plant nutrients (macro and micro nutrients) and bio-fertilizers (beneficial microbes) is key to improve soil organic carbon and field crops productivity. The best management practices that increase SOC could reduce soil pollution and improve the health of all on the earth[70]. According to Lal,[71] field crop production in Africa, Asia and South America could be increased by millions every year, by increasing soil organic matter by one ton per hectare.

      The variations in the TCC estimated for different countries and it's partitioning into roots (BCC) and shoots (ACC) may be attributed to the differences in the genetic make of the crop varieties used in different countries, the variation in the environmental conditions among the countries, and different agronomic practices used in different countries. The review of global data[72] showed that TCC transfer was highest in maize, which yielded the greatest soil C sequestration potential (1.0 Mg C ha−1 yr−1 or 19% total assimilation), followed by sorghum (1.0 Mg C ha−1, 17%) and wheat (0.8 Mg C ha−1 yr−1, 23%). Variation in TCC among cereals such as maize, sorghum, wheat and rice has been earlier reported by McKendry[73]. According to Zengeni et al.[72] higher TCC transfer to soils occurred under clayey soils and warmer climates provided that exudation is high enough to offset respiration C losses. According to Ma et al.[21], plant organ C content is 45.0% in reproductive organs, 47.9% in stems, 46.9% in leaves and 45.6% in roots.

      For increasing TCC accumulation in plants and it's partitioning into ACC and BCC it is important to (1) select high yielding plants genotypes, (2) use best agronomic (management) practices and (3) planting of crops in suitable environmental conditions. The best agronomic practices that improve crop growth and development, increase grain and total biomass thus increase TCC in different crop species (Tables 58). Any biotic or abiotic stress that could reduce the productivity (yield or biomass) of field crops could reduce the TCC and its partitioning into ACC and BCC under different environments. The agronomists study various crop production problems and work for better soil and crop management practices to obtain higher yield[74].

    • The increase in carbon sequestration (1 kg of carbon is equal to 3.67 kg of CO2) through the process of photosynthesis in field crops is essential to combat the issue of food security and global warming. However, the lack of simplified and easy way of carbon estimation restricts researchers to estimate data on total carbon content (TCC) sequestered or captures by the field crops and it's partitioning into roots and shoots. In this study, highly simplified calculations have been developed to provide easy estimation of carbon content in below-ground parts (BCC) and above-ground parts (ACC) of various field crops, including wheat, rice, maize, barley, and more. Best agronomic practices that improve or increase the rate of photosynthesis under field conditions significantly increase the capture or sequestration carbon. Crops with higher TCC took more CO2 (higher photosynthetic efficiency) from the atmosphere therefore increase the yield per unit area and decrease the negative impacts of global warming and food security. The simplified approach for carbon content (CC) estimation utilized in this study can be highly beneficial for researchers and students. It allows for easy estimation of the carbon content fixed in the roots and shoots of diverse field crops, including wheat, rice, maize, and barley. The total carbon content (TCC) in plants exhibited a positive correlation with total biomass. Furthermore, both below-ground carbon content (BCC) and above-ground carbon content (ACC) demonstrated a positive association with TCC. It was confirmed from the model, that out of the total 100% TCC accumulation by field crops, 82% is partitioned into ACC (shoots) and 18% into BCC (roots). The practices that increase grain yield, harvest index, and total biomass increased carbon content in roots and shoots of different crop species. The best agronomic practices that increase grain yield in field crops per unit area will also increase the TCC accumulation and it's portioning into ACC and BCC. Selecting carbon superior genotypes of crop species along with best management practices including sustainable soil management practices will significantly reduce CO2 emission and increase soil health, productivity and sustainability with more carbon sequestration into the soils.

      • The author declares that there is no conflict of interest.

      • Copyright: © 2023 by the author(s). Published by Maximum Academic Press, Fayetteville, GA. This article is an open access article distributed under Creative Commons Attribution License (CC BY 4.0), visit https://creativecommons.org/licenses/by/4.0/.
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    Amanullah. 2023. A simple model for estimation of above and below ground carbon in cereal crops. Technology in Agronomy 3:8 doi: 10.48130/TIA-2023-0008
    Amanullah. 2023. A simple model for estimation of above and below ground carbon in cereal crops. Technology in Agronomy 3:8 doi: 10.48130/TIA-2023-0008

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