globalchange  > 过去全球变化的重建
DOI: 10.1371/journal.pone.0166536
论文题名:
Variations in Soil Microbial Biomass Carbon and Soil Dissolved Organic Carbon in the Re-Vegetation of Hilly Slopes with Purple Soil
作者: Ning Yang; Dongsheng Zou; Manyuan Yang; Zhonggui Lin
刊名: PLOS ONE
ISSN: 1932-6203
出版年: 2016
发表日期: 2016-12-15
卷: 11, 期:12
语种: 英语
英文关键词: Soil ecology ; Carbon sequestration ; Paleopedology ; Soil chemistry ; Community ecology ; Soil respiration ; Biomass (ecology) ; Plant communities
英文摘要: Crust restoration is increasingly being done but we lack quantitative information on soil improvements. The study aimed to elucidate the dynamics involving soil microbial biomass carbon and soil dissolved organic carbon in the re-vegetation chronosequences of a hillslope land with purple soil in Hengyang, Hunan Province. The soil can cause serious disasters with both soil erosion and seasonal drought, and also becomes a typical representative of ecological disaster area in South China. Using the space-for-time method, we selected six typical sampling plots, designated as follows: grassplot community, meadow thicket community, frutex community, frutex and arbor community, arbor community, and top-level vegetation community. These plots were established to analyze the changes in soil microbial biomass carbon, soil microbial quotien, dissolved organic carbon, dissolved organic carbon/soil organic carbon, and soil basal respiration in 0–10, 10–20, and 20–40 cm soil layers. The relationships of these parameters with soils physic-chemical properties were also determined. The ecological environment of the 6 plant communities is similar and typical; they denoted six different successive stages of restoration on hillslopes with purple soils in Hengyang, Hunan Province. The soil microbial biomass carbon and soil basal respiration contents decreased with increasing soil depth but increased with re-vegetation. By contrast, soil microbial quotient increased with increasing soil depth and re-vegetation. From 0–10 cm soil layer to 20–40 cm soil layer, the dissolved organic carbon content decreased in different re-vegetation stages. In the process of re-vegetation, the dissolved organic carbon content increased in the 0–10 and 10–20 cm soil layers, whereas the dissolved organic carbon content decreased after an initial increase in the 20–40 cm soil layers. Meanwhile, dissolved organic carbon/soil organic carbon increased with increasing soil depth but decreased with re-vegetation. Significant correlations existed among soil microbial biomass carbon, soil microbial quotient, dissolved organic carbon, soil basal respiration and soil physic-chemical properties associated with soil fertility. The results showed that re-vegetation was conducive to the soil quality improvement and the accumulation of soil organic carbon pool of the hillslope land with purple soil in Hengyang, Hunan Province.
URL: http://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0166536&type=printable
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/23402
Appears in Collections:过去全球变化的重建
影响、适应和脆弱性
科学计划与规划
气候变化与战略
全球变化的国际研究计划
气候减缓与适应
气候变化事实与影响

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作者单位: College of Landscape Architecture, Hunan Environmental-Biological Polytechnic College, Hengyang, China;College of Bioscience and Biotechnology, Hunan Agricultural University, Changsha, China;College of Bioscience and Biotechnology, Hunan Agricultural University, Changsha, China;College of Landscape Architecture, Hunan Environmental-Biological Polytechnic College, Hengyang, China;College of Landscape Architecture, Hunan Environmental-Biological Polytechnic College, Hengyang, China

Recommended Citation:
Ning Yang,Dongsheng Zou,Manyuan Yang,et al. Variations in Soil Microbial Biomass Carbon and Soil Dissolved Organic Carbon in the Re-Vegetation of Hilly Slopes with Purple Soil[J]. PLOS ONE,2016-01-01,11(12)
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