SavedAdd your journal

Journals / Tarım Bilimleri Dergisi / 2022 / Cilt: 28 - Sayı: 3

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

İbrahim Halil YANARDAG
Asuman BÜYÜKKILIÇ YANARDAĞ
Ahmet Ruhi MERMUT
Angel FAZ CANO
Pages
501–510
Publication Date
2022-09-05
DOI
—
🏛️Bibliographic metadata and full text access for this article are provided via DergiPark.
DergiPark Record ↗
✨

AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

Stable organic matter content was significantly related to clay content and greatly influenced by the type of soil management used.

📌 3 Key Takeaways

🎯
Objective & Hypothesis: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.
📊
Key Findings & Data: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.
💡
Conclusion & Impact:Stable organic matter content was significantly related to clay content and greatly influenced by the type of soil management used.
🔬Design:Research Article
📍Scope:2000 Verileri
⚙️Variables:Soil organic carbon · Soil inorganic carbon · carbon storage

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.

🔖

Cite This Article

YANARDAG, İ. H., YANARDAĞ, A. B., MERMUT, A. R., CANO, A. F. (2022). Carbon Storage Potential and its Distributions in the Particle Size Fractions in Harran Plain, Turkey. Tarım Bilimleri Dergisi, Cilt: 28 - Sayı: 3, 501–510. https://ajindex.com/articles/702576

📄 Full Text PDF Viewer

📄

PDF görüntüleyici hazırlanıyor...

References (7)

  1. 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
  2. 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
  3. 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
  4. 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
  5. 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
  6. 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
  7. 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 & Stangenber