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Response of Soil Microbes to Vegetation Restoration in Coal Mining Subsidence Areas at Huaibei Coal Mine, China

机译:中国淮北煤矿煤矿沉积地区土壤微生物对植被恢复的反应

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摘要

Vegetation restoration is an available way to ameliorate degraded lands. In order to study the response of soil microbes to vegetation restoration in coal mining subsidence areas, the composition and distribution of soil microbes were discussed through three plots: unsubsided area (CA), new subsided area (NSA), and old subsided area (OSA) with different vegetation restoration time in Huabei coal mine. Meanwhile, changes in soil catalase and urease activity were explored and the correlation between soil bacteria, fungi, and environmental factors was analysed. The results demonstrated that Nitrospira was the dominant bacteria in all areas sampled. Microorganisms in the 0–20 cm and 40–60 cm soil layers of OSA had the highest Simpson index, whereas the index in NSA was lowest (at all soil depths). The catalase activity in NSA was significantly higher than that in CA, and there was no significant difference in catalase activity with soil depth, while the urease activity declined gradually with increasing soil depth. The urease activity in the 20–60 cm soil layer of NSA and OSA was significantly higher than that of CA. Furthermore, the distribution of bacteria was mainly affected by soil organic matter, available potassium, available phosphorus, and alkali-hydrolyzable nitrogen, whereas pH and catalase activity mainly affected fungal distribution. These results implied that soil catalase activity in NSA and urease activity in the 20–40 cm soil layer of NSA and OSA were significantly enhanced after vegetation restoration, and that long-term plant restoration could improve soil fertility and soil microbial community diversity in coal mining areas.
机译:植被恢复是改善退化土地的可用方式。为了研究土壤微生物对煤矿沉降区植被恢复的响应,通过三个地块讨论了土壤微生物的组成和分布:未被维护地区(CA),新的消退区(NSA)和旧区区(OSA) )在淮北煤矿的不同植被恢复时间。同时,探讨了土壤过敏酶和脲酶活性的变化,分析了土壤细菌,真菌和环境因素之间的相关性。结果表明,Nitrospira是所有区域采样的主要细菌。 0-20厘米和40-60厘米的OSA土层中的微生物具有最高的辛普森指数,而NSA的指数最低(在所有土壤深度)。 NSA中的过氧化氢酶活性显着高于Ca,并且具有土壤深度的过氧化氢酶活性没有显着差异,而土壤深度增加逐渐下降。 NSA和OSA的20-60厘米土壤层中的脲酶活性显着高于CA.此外,细菌的分布主要受土壤有机物质,可用钾,可用磷和碱水解氮的影响,而pH和过氧化氢酶活性主要受到真菌分布。这些结果暗示NSA和OSA的20-40cm土层中NSA和脲酶活性的土壤过缩酶活性显着提高,并且长期植物恢复可以改善煤炭矿业土壤肥力和土壤微生物群落多样性地区。

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