首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Soil and vegetation development along a 10-year restoration chronosequence in tailing dams in the Xiaoqinling gold region of Central China
【24h】

Soil and vegetation development along a 10-year restoration chronosequence in tailing dams in the Xiaoqinling gold region of Central China

机译:中国中华民族萧青金金地区尾坝尾坝沿10年恢复慢素植被发展

获取原文
获取原文并翻译 | 示例
           

摘要

Gold mining has increased sharply in response to global demand. Gold extraction usually causes the formation of tailing dams, in which organic matter and microbial activity decrease, and this consequently constrains plant growth. However, a full understanding of plant-soil interaction and plant community development in terms of natural restoration of gold mine tailing dam has not yet been developed. Three tailing dams, which had been naturally restored for 2 (R2), 5 (R5), and 10 (R10) years in the Xiaoqinlin gold region of Central China, were chosen to explore soil and plant community development in August, 2015. This study showed that soil bulk density and pH value were the lowest, whereas soil organic carbon, total nitrogen, microbial biomass carbon and nitrogen were the highest in the R10 tailing dam across two soil depths (0-10 cm and 10-20 cm). Soil organic carbon, total nitrogen, microbial biomass carbon and nitrogen decreased with soil depth across the restoration periods. The highest ratio of soil organic carbon to total nitrogen in the R10 tailing dam suggests that the rate of soil organic carbon accumulation may be restricted by the total nitrogen content in the long-term. Restoration stimulated plant community diversity and productivity, due to increment in soil nutrient content and microbial biomass carbon and nitrogen. The various ratios of root biomass to aboveground plant biomass among three tailing dams were caused by the shifting of the plant community composition from annual to perennial varietals. The mechanism by which plant-soil interaction and plant community composition change over time can be used to guide restoration programs in tailing dams in Central China.
机译:由于全球需求,金矿急剧增加。金提取通常会导致尾矿坝的形成,其中有机物和微生物活性降低,这因此限制了植物生长。然而,尚未开发出对金矿尾巴大坝的自然恢复方面的植物土相互作用和植物界的全面了解。选择了三个尾矿坝,其自然恢复为2(R2),5(R5)和10岁,在中国中美洲小桥金地区,探讨了2015年8月的土壤和植物群落发展。这个研究表明,土壤堆积密度和pH值是最低的,而土壤有机碳,总氮,微生物生物量碳和氮在两个土壤深度(0-10厘米和10-20厘米)上是最高的R10拖尾坝。土壤有机碳,总氮,微生物生物量碳和氮气在恢复时期的土壤深度下降。土壤有机碳与R10尾矿坝上的总氮的比例最高表明,土壤有机碳积累的速率可能受到长期总氮含量的限制。由于土壤养分含量和微生物生物质碳和氮气增加,恢复刺激植物群落多样性和生产率。三个拖尾水坝中根生物质到地上植物生物质的各种比率是由植物群族组成从年生常数变化引起的。植物 - 土壤相互作用和植物群落组成随时间变化的机制可用于指导中国中部尾坝中的恢复方案。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号