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首页> 外文期刊>Environmental Management >Dump Stability and Soil Fertility of a Coal Mine Spoil in Indian Dry Tropical Environment: A Long-Term Study
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Dump Stability and Soil Fertility of a Coal Mine Spoil in Indian Dry Tropical Environment: A Long-Term Study

机译:印度干燥热带环境中煤矿弃土场的排土场稳定性和土壤肥力:一项长期研究

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摘要

Plant available nitrogen, belowground (root) biomass, soil nitrogen (N) mineralization and microbial biomass N (MBN) were studied for 12 years at the interval of 2 years (0, 2, 4, 6, 8, 10 and 12 years) and mine dump stability at the intervals of 6 years (0, 6 and 12 years) after re-vegetation on coal mine spoil site. Plant available nitrogen in revegetated mine spoil ranged from 4.51 to 6.59 μg g~(-1), net N-mineralization from 1.87 to 13.85 μg g~(-1) month~(-1), MBN from 10 to 22.63 μg g~(-1), and root biomass from 28 to 566 g~(-2). Mining activity has caused a change in soil characteristics including plant available nutrients like nitrate-N, ammonium-N and phos-phate-P by 70, 67, and 76 %, respectively, N-mineralization by 93 %, root biomass values by 97 % and MBN values by 91 % compared to forest ecosystems. Revegetation of mine spoil produced increase in root biomass values by 1.3, 7.6 and 17.2 times, mineral N values by 1.22, 1.43 and 1.79 times, N-mineralization values by 1.8, 5.2 and 12.6 times and MBN values by 1.6, 2.0, and 3.4 times in 2, 6 and 12 years, respectively. Below ground biomass was highly co-related with microbial biomass and plant available nutrients. N-mineralization, plant available nutrients and the clay content were positively correlated with age of revegetation (P < 0.01). From the numerical modelling it was analyzed that revegetation increased the dump slope stability with a factor of safety of 1.7 and 2.1 after 6 and 12 years of plantation on dump slope, respectively, while it was 1.2 before revegetation. Thus, long term revegetation was found to have direct impact on dump stability and indirect impact on soil fertility status in mine spoil, where plant biomass and microbial biomass provide major contributions in ecological redevelopment of the mine spoil.
机译:以2年(0、2、4、6、8、10和12年)的间隔研究了12年的植物有效氮,地下(根)生物量,土壤氮(N)矿化和微生物生物量N(MBN)。在煤矿弃土场重新植被后的6年(0、6和12年)间隔内,矿山倾卸物的稳定性。植被矿化土壤中的植物有效氮为4.51至6.59μgg〜(-1),净氮矿化为1.87至​​13.85μgg〜(-1)月〜(-1),MBN为10至22.63μgg〜 (-1),根生物量为28至566 g〜(-2)。采矿活动导致土壤特性发生变化,包括植物有效营养素,例如硝酸盐-氮,铵态氮和磷-磷酸盐-P分别增加了70%,67%和76%,氮矿化增加了93%,根生物量增加了97%与森林生态系统相比,%和MBN值降低了91%。矿渣的植被再生使根系生物量值增加了1.3、7.6和17.2倍,矿质氮值增加了1.22、1.43和1.79倍,氮矿化值增加了1.8、5.2和12.6倍,MBN值增加了1.6、2.0和3.4分别在2年,6年和12年内。地下生物量与微生物生物量和植物有效养分高度相关。氮矿化,植物有效养分和黏土含量与植被恢复年龄呈正相关(P <0.01)。从数值模型分析,植被恢复增加了堆放场的稳定性,安全系数分别为1.7和2.1,植被恢复期为6年和12年后为1.2。因此,长期的植被恢复对矿山弃渣场的排土稳定性有直接影响,对土壤肥力状况有间接影响,其中植物生物量和微生物生物量为矿山弃渣的生态重建提供了重要贡献。

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