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土壤化学性质而非活性和潜在活性微生物的丰度控制着土壤酶动力学。

Soil chemical properties rather than the abundance of active and potentially active microorganisms control soil enzyme kinetics.

机构信息

Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, 723 Xingke Rd., Tianhe District, Guangzhou 510650, China.

College of Natural Resources and Environment, Northwest A&F University, Key Laboratory of Plant Nutrition and Agro-environment in Northwest China, Ministry of Agriculture, Yangling 712100, Shaanxi, China.

出版信息

Sci Total Environ. 2021 May 20;770:144500. doi: 10.1016/j.scitotenv.2020.144500. Epub 2021 Jan 19.

Abstract

Soil enzymes secreted by microorganisms play a critical role in nutrient cycling, soil structure maintenance, and crop production. However, understanding of the linkage between soil enzyme kinetics and microbial metabolism and active microbial communities is remarkably limited. In this study, we measured the kinetics of three hydrolase enzymes, active microbial abundance and substrate-induced respiration (SIR) from 21 farmlands differing in their fertilities collected from the Loess Plateau, China. Results showed the high fertility soils had higher total organic carbon (TOC) and nutrient contents, potential microbial activity, the colony-forming units (CFU) of actinomycetes, and values of enzyme V and K than those of low fertility soils. We also observed that the CFU of fungi and other bacterial groups did not change with soil fertility status. Soil chemical properties explained 74.0% of the variance in V and 28.3% of the variance in K, respectively. Whereas, the abundance of main microbial groups and fungi/bacteria ratio only explained 10.2% and 7% of the variance of V and K, respectively. The interactive effect of soil properties and microbial community could explain 20.2% of the variance in K. Our results suggest that the substrate availability would mainly drive enzyme kinetics compared to the abundance of active/potentially active microbes in the farmland soils.

摘要

土壤微生物分泌的土壤酶在养分循环、土壤结构维持和作物生产中起着关键作用。然而,人们对土壤酶动力学与微生物代谢和活性微生物群落之间的联系的理解非常有限。在这项研究中,我们测量了来自中国黄土高原的 21 个肥力不同的农田中三种水解酶的动力学、活性微生物丰度和底物诱导呼吸(SIR)。结果表明,高肥力土壤的总有机碳(TOC)和养分含量、潜在微生物活性、放线菌的菌落形成单位(CFU)以及酶 V 和 K 的值均高于低肥力土壤。我们还观察到,真菌和其他细菌群体的 CFU 并没有随土壤肥力状况而变化。土壤化学性质分别解释了 V 的 74.0%和 K 的 28.3%的变异。而主要微生物群体的丰度和真菌/细菌比例仅分别解释了 V 和 K 的 10.2%和 7%的变异。土壤性质和微生物群落的相互作用可以解释 K 的 20.2%的变异。我们的结果表明,与农田土壤中活性/潜在微生物的丰度相比,底物的可用性将主要驱动酶动力学。

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