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Effect of biological soil crusts on microbial activity in soils of the Tengger Desert (China)

机译:生物土壤结皮对腾格里沙漠土壤微生物活性的影响(中国)

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Soil microbes, as an important biological component of soils, have a function in the formation of soils and soil-remediation processes. This paper aims to analyze effects of biocrusts on soil microbial activities in desert ecosystems. Two sets of samples were collected under biocrusts in April, July, October, 2013, and January, 2014, in natural and revegetated areas of the Tengger Desert. The results showed that biocrusts significantly improved soil physicochemical properties, basal respiration and the quantity of soil alkaline phosphatase, protease, and cellulose, and decreased qCO(2) in vegetated areas. Impact of biocrusts on soil microbial activities also varied, depending on the successional stage of crusts and the restoration age. Soil basal respiration and enzyme activity were obviously higher, but qCO(2) were significantly lower in moss dominated crusts than those dominated by cyanobacteria-lichen. Soil basal respiration and enzyme activity positively correlated with the restoration age, but qCO(2) negatively correlated with the restoration age. Soil basal respiration and enzyme activity were the highest in summer, followed by autumn, and the lowest in spring and winter; whereas, qCO(2) displayed an opposite trend. The study suggests that biocrusts have the ability to improve soil quality and promote soil recovery in vegetated areas of the Tengger Desert. (C) 2017 Elsevier Ltd. All rights reserved.
机译:土壤微生物作为土壤的重要生物成分,在土壤形成和土壤修复过程中具有功能。本文旨在分析生物结皮对沙漠生态系统中土壤微生物活动的影响。 2013年4月,7月,10月和2014年1月,在腾格里沙漠的自然和植被恢复地区,用生物结壳收集了两组样品。结果表明,生物结皮显着改善了土壤理化性质,基础呼吸作用以及土壤碱性磷酸酶,蛋白酶和纤维素的数量,并减少了植被区的qCO(2)。生物结皮对土壤微生物活动的影响也有所不同,这取决于结皮的演替阶段和恢复年龄。苔藓为主的地壳中的土壤基础呼吸和酶活性明显较高,但qCO(2)明显低于蓝藻-地衣为主的土壤。土壤基础呼吸和酶活性与恢复年龄呈正相关,而qCO(2)与恢复年龄呈负相关。夏季土壤基础呼吸和酶活性最高,其次是秋季,春季和冬季最低。而qCO(2)显示相反的趋势。研究表明,生物硬皮具有改善腾格沙漠植被地区土壤质量和促进土壤恢复的能力。 (C)2017 Elsevier Ltd.保留所有权利。

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