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Response of Soil Chemical and Microbial Properties to Vegetation Restoration on the Loess Plateau, China

机译:黄土高原地区土壤化学和微生物特性对植被恢复的响应

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摘要

Revegetation has been reported as one of the most effective measures for reducing soil erosion on theLoess Plateau in China. We evaluated the effect of natural revegetation restoration on soil chemicalnutrient, microbial biomass and enzyme activities on the Loess Plateau of China. The vegetation typesstudied, in order from the shortest to the longest enclosure duration, were abandoned grazed grassland(Ab.G3, 3 years), Hierochloe odorata Beauv. (Hi.O7, 7 years) communities, Thymus mongolicus Ronnm(Th.M15, 15 years), Artemisia sacrorum Ledeb (At.S25, 25 years), Stipa bungeana Trin Ledeb (St.B36,36 years), and Stipa grandis P. Smirn (St.G56, 56 years). The results showed that soil organic carbon(SOC) and total nitrogen (N) was 9.2-32.2 and 1.2-3.5 g/kg during vegetation restoration, respectively.Except from Th.M15, SOC and total N increased with restoration time. Also, soil microbial biomass carbon(Cmic), phosphorus (Pmic), invertase activities, and alkaline phosphatase activities increased withrestoration time. Whereas, soil microbial biomass nitrogen (Nmic) and urease activity was the highest inthe early succession period and lowest in the mid succession period (under Th.M15 and At.S25).Revegetation resulted in more abundant and stable soil ecological environment by enhancing soil nutrientsand biological properties. Thus, this is a beneficial measure for the recovery of degraded soils on theLoess Plateau of China.
机译:据报道,植被恢复是减少黄土高原土壤侵蚀的最有效措施之一。我们评估了天然植被恢复对中国黄土高原土壤化学养分,微生物生物量和酶活性的影响。研究的植被类型从最短到最长围封时间依次为废弃的放牧草地(Ab.G3,3年),Hierochloe odorata Beauv。 (Hi.O7,7年),百里香(Th.mus mongolicus Ronnm)(Th.M15,15年),years蒿(At.S25,25年),Stipa bungeana Trin Ledeb(St.B36,36岁)和Stipa grandis P.史米尔(St.G56,56岁)。结果表明,植被恢复过程中土壤有机碳(SOC)和总氮(N)分别为9.2-32.2和1.2-3.5 g / kg。除Th.M15外,SOC和总氮均随着恢复时间的增加而增加。同样,土壤微生物生物量碳(Cmic),磷(Pmic),转化酶活性和碱性磷酸酶活性随恢复时间的增加而增加。土壤微生物生物量氮(Nmic)和脲酶活性在演替初期最高,在演替中期最低(Th.M15和At.S25以下),植被通过强化土壤而导致更丰富和稳定的土壤生态环境。营养和生物学特性。因此,这是恢复黄土高原退化土壤的有益措施。

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