Research Article
BibTex RIS Cite
Year 2022, Volume: 28 Issue: 3, 501 - 510, 05.09.2022
https://doi.org/10.15832/ankutbd.907173

Abstract

References

  • Accoe F, Boeckx P, Van Cleemput O, Hofman, G X, Hui H Bin, & Guanxiong C (2002). Characterization of soil Organic Matter Fraction from Grassland and Cultivated Soils via C Content and δ13C Signature. Rapid Commun Mass Spectrom 16: 2157-2164
  • Batjes N H (1996). Total carbon and nitrogen in the soils of the world. European Journal of Soil Science 47: 151–163 Bongiovanni M D & Labartini J C (2006). Particulate organic matter, carbonhydrate, humic acid contents in soil macro- and microaggregates as affected by cultivation. Geoderma 133: 660-665
  • Bower C A & Wilcox L V (1965). Soluble salts In C A Black (Ed) Methods of Soils Analysis. Madison, Wisconsin, USA, American Society of Agronomy 2: 933-940
  • Carter M R, Angers D A, Gregorich E G & Bolinder MA (2003). Characterizing organic matter retention for surface soils in eastern Canada using density and particle size fractions. Canadian Journal of Soil Science 83: 11–23
  • Chan Y (2008). Increasing soil carbon of agricultural land. NSW DPI Primefact 735
  • Chapman H D (1965). Cation Exchange Capacity. In: Black C A (ed) Methods of Soil Analysis American Society of Agronomy. Madison, Wisconsin, USA 2: 891-900
  • Chen J S & Chiu C Y (2003). Characterization of soil organic matter in different particle-size fractions in humid subalpine soils by CP/MAS 13C NMR. Geoderma 117: 129–141
  • Chenu C, Le Bissonnais Y & Arrouays D (2000). Organic matter influence on clay wettability and soil aggregate stability. Soil Science Society of America Journal 64: 1479-1486
  • Dalal R C & Mayer R J (1986). Long-term trends in fertility of soils under continuous cultivation and cereal cropping in southern Queensland: IV Loss of organic carbon from different density fractions. Aust J Soil Res 24: 293–300
  • DSI (2003). Problems of drainage and salinity in the Harran plain Summary Report, the 15th District Directorate of the State Hydraulic Works, Şanlıurfa, Turkey, 10 (in Turkish)
  • Duchaufour P H (1970) Precis de Pedologie. Masson Paris 481
  • FAO–ISRIC (1990). Guidelines for soil description 3rd edit FAO Roma, 70
  • Figueiredo C C, Resck D V S & Carneiro M A C (2010). Labile and stable fractions of soil organic matter under management systems and native cerrado. Revista Brasileira de Ciência do Solo 34(3): 907-916
  • Gocke M, Pustovoytov K & Kuzyakov Y (2012). Pedogenic carbonate formation: Recrystallization versus migration—Process rates and periods assessed by 14C labeling. Global Biogeochemical Cycle, Volume 26 (1)
  • Homann P S, Sollins P, Chappell H N & Stangenberger A G (1995). Soil organic carbon in a mountainous, forested region: relation to site characteristics. Soil Science Society of America Journal 59: 1468– 1475
  • Hontoria C, Rodriguez-Murillo J C & Saa A (1999). Relationships between soil organic carbon and site characteristics in peninsular Spain. Soil Science Society of America Journal 63: 614–621
  • Khademi H & Mermut A R (1998). Source of palygorskite in gypsiferous Aridisols and associated sediments from Central Iran. Clay Minerals 33: 561–578
  • Li C, Qiu J, Frolking S, Xiao X, Salas W, Moore III B, Boles S, Huang Y & Sass R (2002). Reduced methane emissions from large scale changes in water management of China's rice paddies during 1980–2000. Geophys Res Lett 29 (20)
  • Marinari S, Dell’Abate M T, Brunetti G & Dais C (2010). Differences of stabilized organic carbon fraction and microbiological activity along Mediterranean Vertisols and Alfisols profiles. Geoderma 156: 379–388
  • Mermut A R, Amundson R & Cerling T E (2000). The use of stable isotopes in studying carbonates dynamics in soils. In: Lal R, Kimble JM, Eswaran H & Stewart BA, Editors, Global Climate Change And Pedogenic Carbonates, CRC Press, USA, 65–85
  • Milne E (2008). Soils, Land-use and land-cover change, Natural resource management and policy and Climate change. wwweoearthorg/article/Soil_organic_carbon
  • Peech M (1965). Hidrogen-ion activity. In Black C A (Ed). Methods of Soil Analysis. American Society of Agronomy Madison, Wisconsin, USA 2: 914-916
  • Puget P, Chenu C & Balesdent J (1995). Total and young organic matter distributions in aggregates of silty cultivated soils. Eur J Soil Sci 46: 449–459

Carbon Storage Potential and its Distributions in the Particle Size Fractions in Harran Plain, Turkey

Year 2022, Volume: 28 Issue: 3, 501 - 510, 05.09.2022
https://doi.org/10.15832/ankutbd.907173

Abstract

In recent years, there has been increasing international interest in increasing and sustainably managing soil C stocks to contribute to combating climate change and support food security. In this context, determining the C storage capacity of soils and examining the distribution of soil C based on fractions is of great importance for a better understanding of C dynamics. The present study investigated the storage potential of soil organic carbon (SOC), inorganic carbon (SIC) and total carbon (TC) in 16 selected profiles, and SOC and SIC distribution in five different particle size fractions (2000-425μm, 425-150 μm, 150-106 μm, 106-75 μm, <75 μm) of the Harran plain in Turkey. The results revealed that the particle size distribution in the surface layer varied in the following order depending on soil weight: 850-250> 2000-850> 250-150> 150-75> 75 μm. The organic C content of the soils is low due to the semi-arid climate conditions. Fraction-based soil SOC distribution was in the following order: 11% at 2000-850 μm, 15% at 850-250 μm, 21% at 250-150 μm, 23% at 150-75 μm and <75 μm 30%. Organic matter fractions differed according to the particle size distribution and the applicable soil management system. Stable organic matter content was significantly related to clay content and greatly influenced by the type of soil management used.

References

  • Accoe F, Boeckx P, Van Cleemput O, Hofman, G X, Hui H Bin, & Guanxiong C (2002). Characterization of soil Organic Matter Fraction from Grassland and Cultivated Soils via C Content and δ13C Signature. Rapid Commun Mass Spectrom 16: 2157-2164
  • Batjes N H (1996). Total carbon and nitrogen in the soils of the world. European Journal of Soil Science 47: 151–163 Bongiovanni M D & Labartini J C (2006). Particulate organic matter, carbonhydrate, humic acid contents in soil macro- and microaggregates as affected by cultivation. Geoderma 133: 660-665
  • Bower C A & Wilcox L V (1965). Soluble salts In C A Black (Ed) Methods of Soils Analysis. Madison, Wisconsin, USA, American Society of Agronomy 2: 933-940
  • Carter M R, Angers D A, Gregorich E G & Bolinder MA (2003). Characterizing organic matter retention for surface soils in eastern Canada using density and particle size fractions. Canadian Journal of Soil Science 83: 11–23
  • Chan Y (2008). Increasing soil carbon of agricultural land. NSW DPI Primefact 735
  • Chapman H D (1965). Cation Exchange Capacity. In: Black C A (ed) Methods of Soil Analysis American Society of Agronomy. Madison, Wisconsin, USA 2: 891-900
  • Chen J S & Chiu C Y (2003). Characterization of soil organic matter in different particle-size fractions in humid subalpine soils by CP/MAS 13C NMR. Geoderma 117: 129–141
  • Chenu C, Le Bissonnais Y & Arrouays D (2000). Organic matter influence on clay wettability and soil aggregate stability. Soil Science Society of America Journal 64: 1479-1486
  • Dalal R C & Mayer R J (1986). Long-term trends in fertility of soils under continuous cultivation and cereal cropping in southern Queensland: IV Loss of organic carbon from different density fractions. Aust J Soil Res 24: 293–300
  • DSI (2003). Problems of drainage and salinity in the Harran plain Summary Report, the 15th District Directorate of the State Hydraulic Works, Şanlıurfa, Turkey, 10 (in Turkish)
  • Duchaufour P H (1970) Precis de Pedologie. Masson Paris 481
  • FAO–ISRIC (1990). Guidelines for soil description 3rd edit FAO Roma, 70
  • Figueiredo C C, Resck D V S & Carneiro M A C (2010). Labile and stable fractions of soil organic matter under management systems and native cerrado. Revista Brasileira de Ciência do Solo 34(3): 907-916
  • Gocke M, Pustovoytov K & Kuzyakov Y (2012). Pedogenic carbonate formation: Recrystallization versus migration—Process rates and periods assessed by 14C labeling. Global Biogeochemical Cycle, Volume 26 (1)
  • Homann P S, Sollins P, Chappell H N & Stangenberger A G (1995). Soil organic carbon in a mountainous, forested region: relation to site characteristics. Soil Science Society of America Journal 59: 1468– 1475
  • Hontoria C, Rodriguez-Murillo J C & Saa A (1999). Relationships between soil organic carbon and site characteristics in peninsular Spain. Soil Science Society of America Journal 63: 614–621
  • Khademi H & Mermut A R (1998). Source of palygorskite in gypsiferous Aridisols and associated sediments from Central Iran. Clay Minerals 33: 561–578
  • Li C, Qiu J, Frolking S, Xiao X, Salas W, Moore III B, Boles S, Huang Y & Sass R (2002). Reduced methane emissions from large scale changes in water management of China's rice paddies during 1980–2000. Geophys Res Lett 29 (20)
  • Marinari S, Dell’Abate M T, Brunetti G & Dais C (2010). Differences of stabilized organic carbon fraction and microbiological activity along Mediterranean Vertisols and Alfisols profiles. Geoderma 156: 379–388
  • Mermut A R, Amundson R & Cerling T E (2000). The use of stable isotopes in studying carbonates dynamics in soils. In: Lal R, Kimble JM, Eswaran H & Stewart BA, Editors, Global Climate Change And Pedogenic Carbonates, CRC Press, USA, 65–85
  • Milne E (2008). Soils, Land-use and land-cover change, Natural resource management and policy and Climate change. wwweoearthorg/article/Soil_organic_carbon
  • Peech M (1965). Hidrogen-ion activity. In Black C A (Ed). Methods of Soil Analysis. American Society of Agronomy Madison, Wisconsin, USA 2: 914-916
  • Puget P, Chenu C & Balesdent J (1995). Total and young organic matter distributions in aggregates of silty cultivated soils. Eur J Soil Sci 46: 449–459
There are 23 citations in total.

Details

Primary Language English
Journal Section Makaleler
Authors

İbrahim Halil Yanardag 0000-0003-2558-9600

Asuman Büyükkılıç Yanardağ 0000-0003-3236-1532

Ahmet Ruhi Mermut This is me 0000-0001-7876-6215

Angel Faz Cano This is me 0000-0002-9271-9818

Publication Date September 5, 2022
Submission Date April 1, 2021
Acceptance Date October 9, 2021
Published in Issue Year 2022 Volume: 28 Issue: 3

Cite

APA Yanardag, İ. H., Büyükkılıç Yanardağ, A., Mermut, A. R., Faz Cano, A. (2022). Carbon Storage Potential and its Distributions in the Particle Size Fractions in Harran Plain, Turkey. Journal of Agricultural Sciences, 28(3), 501-510. https://doi.org/10.15832/ankutbd.907173

Journal of Agricultural Sciences is published open access journal. All articles are published under the terms of the Creative Commons Attribution License (CC BY).