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毗邻新建湖泊的草原土壤理化及微生物特性的空间格局。

Spatial patterns in soil physicochemical and microbiological properties in a grassland adjacent to a newly built lake.

机构信息

Department of Grassland Science, College of Animal Science and Technology, China Agricultural University, Beijing, China.

Department of Soil and Water Science, College of Resources and Environment Sciences, China Agricultural University, Beijing, China.

出版信息

Microbiologyopen. 2019 Dec;8(12):e912. doi: 10.1002/mbo3.912. Epub 2019 Aug 31.

DOI:10.1002/mbo3.912
PMID:31472010
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6925176/
Abstract

Soil water content (SWC) is an important determinant for nutrient cycling and microorganism activity in the grassland ecosystem. Lakes have a positive effect on the water supply of the neighboring ecosystem. However, information evaluating whether newly built lakes improve the physiochemical properties and microorganism activity of adjacent grassland soil is rare. A 15-hectare artificial lake with a 2 m depth was built on grazed grassland to determine whether the change of soil physiochemical properties and microorganism activity of the adjacent grassland depended on the distance from the lake. SWC and total nitrogen (TN) were greater within 150 m of the lake than at distances over 150 m from the lake. The total organic carbon (TOC) increased first at 100-150 m from the lake and then decreased. The soil microbial biomass and the bacterial and fungal contents increased with increasing years after the construction of the lake. Gram-negative bacteria and methanotrophic bacteria were greater within a 30 m distance of the lake. Over 60 m away from the lake, Actinobacteria, gram-positive bacteria, and anaerobic bacteria showed higher abundances. In the area near the lake (<250 m distance), microorganisms were strongly correlated with SWC, EC, TN, and TOC and greatly correlated with the changes of total phosphorous (TP) and pH when the distance from the lake was over 250 m. The results indicated that the newly built lake could be a driving factor for improving the physiochemical properties and microorganism activity of adjacent grassland soil within a certain range.

摘要

土壤含水量(SWC)是草原生态系统中养分循环和微生物活动的重要决定因素。湖泊对邻近生态系统的供水有积极影响。然而,评估新建湖泊是否改善邻近草原土壤的理化性质和微生物活性的信息很少。在放牧草原上建造了一个 15 公顷、深 2 米的人工湖,以确定土壤理化性质和微生物活性的变化是否取决于距离湖泊的远近。SWC 和总氮(TN)在距湖泊 150 米以内的区域大于距湖泊 150 米以上的区域。总有机碳(TOC)在距湖泊 100-150 米处首先增加,然后减少。土壤微生物生物量以及细菌和真菌含量随着湖泊建成后年份的增加而增加。距湖泊 30 米以内的革兰氏阴性菌和甲烷氧化菌较多。距湖泊 60 米以外,放线菌、革兰氏阳性菌和厌氧菌的丰度较高。在靠近湖泊的区域(<250 米距离),微生物与 SWC、EC、TN 和 TOC 强烈相关,当距离湖泊超过 250 米时,与总磷(TP)和 pH 的变化也密切相关。结果表明,在一定范围内,新建湖泊可能是改善邻近草原土壤理化性质和微生物活性的驱动因素。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6af5/6925176/d558ee664d04/MBO3-8-e912-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6af5/6925176/21664f22b57e/MBO3-8-e912-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6af5/6925176/fbe135313975/MBO3-8-e912-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6af5/6925176/4a24d82b38d1/MBO3-8-e912-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6af5/6925176/9571f6a2de66/MBO3-8-e912-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6af5/6925176/ea83004ba517/MBO3-8-e912-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6af5/6925176/d558ee664d04/MBO3-8-e912-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6af5/6925176/21664f22b57e/MBO3-8-e912-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6af5/6925176/fbe135313975/MBO3-8-e912-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6af5/6925176/4a24d82b38d1/MBO3-8-e912-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6af5/6925176/9571f6a2de66/MBO3-8-e912-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6af5/6925176/ea83004ba517/MBO3-8-e912-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6af5/6925176/d558ee664d04/MBO3-8-e912-g006.jpg

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