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Effects of Climate Changes and Pollution with Heavy Metals on the Transformation of Carbon Compounds in Different Soil Types of Agroecosystems in the Forest-Steppe of Baikal Region

机译:气候变化与重金属污染对百米米森林森林 - 草原不同土壤类型碳化合物转化的影响

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摘要

The results of long-term (1992-2005) monitoring of the carbon compounds transformation in soils of forest- steppe agroecosystems polluted by heavy metals in the Baikal region in the years different from the "climatic norm" are discussed. The influence of environmental factors on the functioning of microbial community was estimated by the C-micr content and CO2 emission. The changes in the ecophysiological parameters (C-micr/C-org and C-CO2/C-micr, mg/(g h) related to the availability of the substrate and intensity of carbon (re)immobilization in different soils revealed the differences in the formation of a stable microbial community dependent on the environmental factors, especially in anomalous years. The use of a systemic approach and analysis of the carbon compounds transformation based on the proportion between the flows of net-mineralized and (re)immobilized carbon (NM: RI) allowed to evaluate integrally the functioning regime of the agroecosystems and the ecological impact on them. The differences in the functioning of agroecosystems on different heavy metal-polluted soils identified on the background of climatic changes are suitable for forecasting the current state and development of agroecosystems. For agroecosystems of this region, C-CO2 emission was estimated for the first time; it was more intense from the soils with the high humus content than from the soils poor in humus (141 and 101 g C/m(2), respectively).
机译:讨论了长期(1992-2005)监测森林 - 草原农鸡系统的碳化合物转化的碳化合物在不同于“气候常态”的百年米米米米米米米米的农业生物系统中的转化。通过C-MIT含量和CO2排放估算了环境因素对微生物群落功能的影响。生态学参数(C-MICR / C-ORG和C-CO2 / C-MICT,MG /(GH)的变化与不同土壤中的碳(RE)固定的底物(RE)固定相关的相关性显示出差异形成稳定的微生物群落,依赖于环境因素,特别是在异常年份。使用基于净矿化和(RE)固定碳流动(NM)的碳化合物转化的系统方法和分析:ri)允许一体地评估农业生物系统的运作制度以及对它们的生态影响。农业体系在气候变化背景上发现的不同重金属污染土壤的运作差异适用于预测当前的国家和发展农业系统。对于该地区的农业系统,第一次估计C-CO2排放;它与高腐殖质的土壤更加激烈T分别从腐殖质(分别为141和101g c / m(2)的土壤。

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