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印度干旱热带地区矿区复垦后生态系统碳库和土壤 CO 通量的变化。

Changes in ecosystem carbon pool and soil CO flux following post-mine reclamation in dry tropical environment, India.

机构信息

Department of Environmental Science and Engineering, Center of Mining Environment, Indian Institute of Technology (Indian School of Mines), Dhanbad 826004, India.

Department of Environmental Science and Engineering, Center of Mining Environment, Indian Institute of Technology (Indian School of Mines), Dhanbad 826004, India.

出版信息

Sci Total Environ. 2017 Apr 1;583:153-162. doi: 10.1016/j.scitotenv.2017.01.043. Epub 2017 Jan 14.

Abstract

Open strip mining of coal results in loss of natural carbon (C) sink and increased emission of CO into the atmosphere. A field study was carried out at five revegetated coal mine lands (7, 8, 9, 10 and 11years) to assess the impact of the reclamation on soil properties, accretion of soil organic C (SOC) and nitrogen (N) stock, changes in ecosystem C pool and soil CO flux. We estimated the presence of C in the tree biomass, soils, litter and microbial biomass to determine the total C sequestration potential of the post mining reclaimed land. To determine the C sequestration of the reclaimed ecosystem, soil CO flux was measured along with the CO sequestration. Reclaimed mine soil (RMS) fertility increased along the age of reclamation and decreases with the soil depths that may be attributed to the change in mine soils characteristics and plant growth. After 7 to 11years of reclamation, SOC and N stocks increased two times. SOC sequestration (1.71MgChayear) and total ecosystem C pool (3.72MgChayear) increased with the age of reclamation (CO equivalent: 13.63MgCOhayear). After 11years of reclamation, soil CO flux (2.36±0.95μmolms) was found four times higher than the natural forest soils (Shorea robusta Gaertn. F). The study shows that reclaimed mine land can act as a source/sink of CO in the terrestrial ecosystem and plays an important role to offset increased emission of CO in the atmosphere.

摘要

露天采煤导致天然碳(C)汇损失和 CO 排放增加到大气中。在五个复垦煤矿区(7、8、9、10 和 11 年)进行了一项实地研究,以评估复垦对土壤特性、土壤有机碳(SOC)和氮(N)储量的积累、生态系统 C 库的变化以及土壤 CO 通量的影响。我们估计了树木生物量、土壤、凋落物和微生物生物量中 C 的存在,以确定矿区复垦后土地的总碳固存潜力。为了确定复垦生态系统的碳固存,我们测量了土壤 CO 通量以及 CO 固存。随着复垦时间的增加,复垦矿区土壤(RMS)肥力增加,而随着土壤深度的增加,肥力下降,这可能归因于矿区土壤特性和植物生长的变化。复垦 7 至 11 年后,SOC 和 N 储量增加了两倍。SOC 固存(1.71MgCha-1 年)和总生态系统 C 库(3.72MgCha-1 年)随着复垦年龄的增加而增加(CO 当量:13.63MgCOha-1 年)。复垦 11 年后,土壤 CO 通量(2.36±0.95μmolms)比天然森林土壤(Shorea robusta Gaertn. F)高四倍。研究表明,复垦矿区土地可以作为陆地生态系统中 CO 的源/汇,并在抵消大气中 CO 排放增加方面发挥重要作用。

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