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Changes of Soil Microbiological Properties during Grass Litter Decomposition in Loess Hilly Region China

机译:黄土丘陵区草凋落物分解过程中土壤微生物学特征的变化

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摘要

Litter, the link between soil and plant, is an important part of nutrient return to soil. Deeply understanding the effect of litter decomposition on soil microbiological properties is important for the sustainable development of grasslands. Three plants (Thymus quinquecostatus Celak., Stipa bungeana Trin. and Artemisia sacrorum ledeb.) leaf litter were selected. A simulation experiment using the nylon bag method was conducted to measure the soil microbial biomass carbon and nitrogen, and soil enzyme activity during litter decomposition. The results showed that the decomposition of three leaf litter enhanced soil microbial carbon and nitrogen. The change rate of soil microbial carbon and nitrogen decreased as Ar.S > St.B > Th.Q. The activities of soil invertase, soil urease, and soil nitrate reductase were significantly improved by the coverage of leaf litter. After 741-day litter decomposition, the change rate of soil invertase was from 16.7% to 33.2%. The change rate of soil urease was highest in the Th.Q treatment; St.B treatment and Ar.S treatment followed, and lowest in the control. The change rates of soil nitrate reductase in the St.B and Ar.S treatment were >1000% higher than those of other treatments. The response of soil enzyme activity to litter decomposition “lagged” behind the change of soil microbial biomass. The significant increase of soil microbial biomass and enzyme activity demonstrated that litter decomposition played an important role in maintaining soil ecological function.
机译:垃圾是土壤与植物之间的联系,是养分返回土壤的重要组成部分。深刻理解凋落物分解对土壤微生物学特性的影响,对于草地的可持续发展具有重要意义。选择了三株植物(百里香,百里香,三角叶青蒿和sa蒿)。进行了使用尼龙袋法的模拟实验,测量了凋落物分解过程中土壤微生物生物量碳和氮以及土壤酶的活性。结果表明,三叶凋落物的分解增强了土壤微生物的碳和氮。土壤微生物碳氮的变化率随着Ar.S> St.B> Th.Q的降低而降低。凋落物的覆盖显着提高了土壤转化酶,土壤脲酶和硝酸盐还原酶的活性。 741天凋落物分解后,土壤转化酶的变化率从16.7%增加到33.2%。 Th.Q处理的土壤脲酶变化率最高。随后进行St.B处理和Ar.S处理,在对照组中最低。 St.B和Ar.S处理的土壤硝酸盐还原酶变化率比其他处理高> 1000%。土壤酶活性对凋落物分解的响应“滞后”于土壤微生物量的变化。土壤微生物量和酶活性的显着增加表明,凋落物分解在维持土壤生态功能中起着重要作用。

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