Soil organic carbon fractions in different land use systems of Chernozem soil

Srđan Šeremešić, L. Nešić, V. Ćirić, J. R. Vasin, I. Đalović, J. Marinković, B. Vojnov
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引用次数: 1

Abstract

The relationship between soil carbon fractions in Chernozem soils was assessed in soil samples of three different environments: arable soil, grassland and oak for?est. Grassland and oak forest had higher soil organic carbon (SOC), carbon soluble in hot water (HWC), particulate organic carbon (POC) and mineral-associated carbon (MOC) than the arable soil. The POC/MOC ratio was lowest in arable soil, indicating a smaller carbon pool for microbial turnover. POC increases with higher total SOC, indicating that the pres?ervation of organic matter depends on the renewal of labile fractions. Our results showed that fertilization had active role in soil carbon stabilization, while crop rotation had less effect on a soil carbon turnover. Our result could contribute to the better understanding of SOC fractions composition and relevance in Chernozem soil, thus could help in selection of cropping management systems for SOC preservation.
黑钙土不同土地利用方式土壤有机碳组分
以黑钙土为研究对象,在耕地、草地和栎树3种不同环境下,评价了黑钙土土壤碳组分之间的关系。草地和栎林土壤有机碳(SOC)、热溶碳(HWC)、颗粒有机碳(POC)和矿物伴生碳(MOC)均高于耕地土壤。耕地土壤的POC/MOC最低,表明微生物周转的碳库较小。POC随着总SOC的增加而增加,表明压力?有机物的观测依赖于不稳定组分的更新。结果表明,施肥对土壤碳稳定有积极作用,而轮作对土壤碳周转影响较小。研究结果有助于更好地了解黑钙土有机碳组分的组成及其相关性,从而有助于选择有利于有机碳保存的耕作管理制度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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