Emine Güler AKGEMCİ, Rasim KOÇYİĞİT, İrfan OĞUZ

Dependency of Soil Organic Carbon Mineralization to Moisture and Temperature under Different Land Uses

Temperature and humidity are the important environmental factors that control the decomposition of organic carbon in the soil. The sensitivity of the soils to temperature and moisture may vary. The aim of this study is to determine the change in mineralized C content of different soils (agriculture, pasture and forest) at different temperature (20 oC and 35 oC) and humidity conditions (30% and 60% of field capacity). This study was carried out in agriculture, forest and pasture lands in Almus district of Tokat province. In the study, soil samples were taken from 0-5, 5-15 and 15-30 cm depths by hand probe. Particle distribution, pH, lime, organic matter, total C, organic C, microbial biomass C and mineralize C were determined in the samples. Mineralize C content was determined by incubation of 30% and 60% of field capacity at 20 oC and 30 oC. Soils were generally classified as clay texture. The highest organic C was found in forest soil. Microbial biomass C showed significant change depending on land use. The difference between the land uses at 20 °C incubation was only observed at 60% of field capacity. The similar trend was also seen at 35 °C temperature. Significant differences have been observed between uses at high humidity conditions. While the increase in the amount of moisture significantly increased the amount of mineralize C in agricultural soil, the increase in temperature in forest soil was significant. This result indicates that the amount of mineralize C in the forest soil is more sensitive to temperature, while agricultural soil is more sensitive to the increase in moisture content.

Keywords:

Land use soil temperature, soil moisture, mineralize C,

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Arslan EI, İpek U, Aslan S, Öbek E (2009). Farklı kompostların topraktaki karbon mineralizasyonu. Anadolu Üniversitesi Bilim ve Teknoloji Dergisi, 10(2):389-395.
Bouyocous GJ (1951). A recalibration of the hydrometer method for making mechanical analysis of soil. Argon. Jour, 43:434-438.
Bowden RD, Newkırk KM, Rullo GM (1998). Carbon dioxide and methane fluxes by aforest soil under labratory-controlled moisture and temperature conditions. Soil Biol. Biochem. 30:1591-1597.
Demirci S (2008). Farklı arazi kullanımlarında agregatlara bağlı karbon ile biyolojik karbon ve azot fraksiyonlarının belirlenmesi. Gaziosmanpaşa Üniversitesi, Fen Bilimleri Enstitüsü, Toprak Anabilim Dalı.
Dinç U, Kapur S, Akça E, Özden M, Senol S, Dingil M, Öztekin E, Kızılarslanoglu HA, Keskin S (2001). History and status of soil survey programmes in Turkey and suggestions on land management. In (P. Zdruli, P. Steduto, C. Lacirignola, L. Montanarella) soil resources of southern and eastern mediterranean countries. options mediterraneennes, Serie B. n. 34. 263-273.
Gudasz C, Bastviken D, Steger K, Premke K, Sobek S (2010). Temperature-controlled organic carbon mineralization in lake sediments. Macmillan Publishers Limited, vol: 466.
Horwath WR, Paul EA (1994). Microbial biomass. Pages 753-773 In Weaver RW, Angle S, Bottomley P, Smith D, Tabatabai S, and A. Wollum, Editors. methods of soil analysis. Part 2. Microbiological and biochemical properties.
IPCC (2000). Land use change and forestry. IPCC, special report. Cambridge University Press: Cambridge.
Jaiyeoba IA (2003). Changes in soil properties due to continuous cultivation in Nigerian semiarid Savannah. Soil and Tillage Research 70:91-98.
Kara Ö, Bolat İ (2008). Bartın ili orman ve tarım topraklarının mikrobiyal biokütle karbon ve azotun içerikleri. Ekoloji 18: 32-40.
Klute A (1986). Water retention: laboratory methods. methods of soil analysis. Part1.2nd Ed. Agronomy 9. Am. Soc. Argon., 635-660, Madison.
Kutlay A, Darıcı C, Aka Sağlıker H (2010). Doğu akdeniz bölgesinde yetişen capparis spinosa l. topraklarında organik madde mineralizasyonu. 3 (3):259-263.
Lal R (2003). Soil erosion and the global carbon budget. Environmental International, 29: 437-450.
Mclaughlin SB and Walsh ME (1998). Evaluating enviromental consequences of producing herbaceous crops for bioenergy. Biomass and Bioenergy. 14: 317-324.
Mohammed AM, Naab JB, Nartey E and Adiku SGK (2014). Carbon mineralization from plant residue-amended soils under varying moisture conditions. Journal of Experimental Biology and Agricultural Sciences. Volume 1 (7 - Special Issue on soil and water management in agriculture).
Oğuz İ and Acar M (2011). Tokat Kazova koşullarında farklı arazi kullanım türlerinin bazı toprak özellikleri üzerine etkisinin araştırılması. Gaziosmanpaşa Üniversitesi, Ziraat Fakültesi Dergisi. 28(2): 171-178.
Pan G, Qu F, Tan S, Smith P, Zhang A, Zhang Q, Li L, Zhang X (2010). Effect of household land management in constraining soil organic carbon storage at plot scale in a red earth soil Area of South China earth soil Area Of South China. 19th World Congress of Soil Science, Soil Solutions for a Changing World 1 – 6 August, Brisbane, Australia. Published on DVD.
Paul EA, Colins HP, Leavilt SW (2001). Dynamics of resistant soil carbon of midwestern agricultural soils measured by naturally occurring C-14 abundance. Geoderma 104:239-256.
Riezebos HT, Loerts AC (1998). Infuence of land use change and tillage practise on soil organic matter southern Brazil and eastern Paraguay. Soil and Tillage Research 49:271-275.
Richards LA (1954). Diagnosis and improvement of saline and alkaline soils, U.S.D.A. Handbook, No:60.
Sağlıker HA (2005). Doğu Akdeniz Bölgesinde iki farklı ana materyalden oluşan toprak üzerinde yetişen Olea Europaea L., Pinus Brutia Ten., Pistacia Terebinthusl.’un bazı ekolojik özelliklerinin mevsimsel değişimlerinin karşılaştırmalı olarak incelenmesi. Çukurova Üniversitesi, Fen Bilimleri Enstitüsü Biyoloji Anabilim Dalı, Doktora Tezi.
Schwendenmann L, Pendall E, Potvin C (2007). Surface soil organic carbon pools, mineralization and CO2 efflux rates under different land-use types in Central Panama. Linking ecological, economic and social constraints of land use and conservation, vol: 107-129.
Zhao WZ, Xiao HL, Liu ZM, Li J (2005). Soil degradation and restoration as affected by land use change in the semiarid Bashang area, Northern China. Catena. 59:173-186.
Zinn Y, Lal R, Resck DVS (2005). Changes in soil organic carbon stocks under agricultura in Brazil. Soil and Tillage Reseach. 84:28-40.

Gaziosmanpaşa Üniversitesi Ziraat Fakültesi Dergisi-Cover

ISSN: 1300-2910
Yayın Aralığı: Yılda 3 Sayı
Başlangıç: 1985
Yayıncı: Tokat Gaziosmanpaşa Üniversitesi Ziraat Fakültesi Dergisi Yayın Ofisi