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黄土区采煤塌陷对土壤全氮和有机质含量空间变异性的影响

张雅馥1,王金满1,2*,祝宇成1   

  1. 1中国地质大学土地科学技术学院, 北京 100083;2国土资源部土地整治重点实验室, 北京 100035)
  • 出版日期:2018-06-10 发布日期:2018-06-10

Effects of land subsidence caused by coal mining on the spatial variation of soil total nitrogen and organic matter concentrations in loess area.

ZHANG Ya-fu1, WANG Jin-man1,2*, ZHU Yu-cheng1   

  1. (1School of Land Science and Technology, China University of Geosciences, Beijing 100083, China; 2Key Laboratory of Land Consolidation and Rehabilitation, Ministry of Land and Resources, Beijing 100035, China).
  • Online:2018-06-10 Published:2018-06-10

摘要: 煤矿开采导致地表塌陷,并改变原有土壤肥力性质。为了更好地开展矿区土地复垦,进行土壤重构和植被重建工作,必须要对塌陷区土壤养分状况进行分析。本研究以山西省朔州市平鲁区安家岭3号井工矿塌陷稳沉区为对象,分层采集原地貌、塌陷区1、塌陷区2和塌陷复垦区的土壤样品,测定不同区域土壤全氮和有机质含量,采用经典统计学和地统计学方法研究了土壤全氮和有机质含量的空间变异性。结果表明:垂直方向上,塌陷区表层0~20 cm土壤全氮和有机质含量小于原地貌,但20 cm以下土壤,塌陷区全氮含量大于原地貌,塌陷区有机质含量小于原地貌。塌陷复垦区的有机质含量大于塌陷区,但塌陷复垦区各层次土壤全氮含量与塌陷区相比,没有呈现一定规律。塌陷增加了土壤有机质和全氮含量在水平方向的分异程度,而土地复垦则降低了土壤有机质和全氮含量在水平方向的变异性。本研究可以为黄土区采煤塌陷地复垦提供一定的理论依据和技术支持。

关键词: 植被指数, 高光谱, 夏玉米, 模型, 干旱, 反射率, 一阶导数, 吸收光合有效辐射比

Abstract: Coal mining causes land subsidence and changes soil fertility. For a better land reclamation in mining area, including soil reconstruction and vegetation restoration, soil nutrient status in subsidence area should be examined. In this study, the subsidence area from Anjialing No. 3 underground coal mine in Pinglu District, Shuozhou City, Shanxi Province was taken as the research area. Soil samples of different profiles from four different plots (unmined area, subsided area 1, subsided area 2, and reclaimed area) were collected to analyze the contents of soil total nitrogen and organic matter. The spatial variation of those characters was examined using classic statistics and geostatistics methods. Soil total nitrogen and organic matter contents at the 0-20 cm layer in the subsided areas were lower than those in the unmined area. However, soil total nitrogen contents at deeper soil layers in the subsided areas were higher than those in the unmined area and an opposite pattern was found for soil organic matter. The soil organic matter content in reclaimed area was higher than that in the subsided areas. Total nitrogen contents at different soil layers in the reclaimed area did not show a clear regularity compared to the subsided areas. Land subsidence increased the variability of soil organic matter and total nitrogen at horizontal direction, whereas land reclamation decreased such spatial variability. Our results can provide a theoretical and technical reference for land reclamation in subsided lands in loess area.

Key words: the first derivative spectral reflectance, drought, vegetation index, summer maize, model., fraction of absorbed photosynthetically active radiation, reflectance, hyperspectral