中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Identifying the mean residence time of soil water for different vegetation types in a water source area of the Yuanyang Terrace, southwestern China

文献类型:期刊论文

作者Ma, Jing1; Song, Weifeng2; Wu, Jinkui3; Liu, Zongbin2; Wei, Zheng4
刊名ISOTOPES IN ENVIRONMENTAL AND HEALTH STUDIES
出版日期2019-05-04
卷号55期号:3页码:272-289
ISSN号1025-6016
关键词Hydrogen-2 isotope hydrology mean residence time oxygen-18 sine-wave regression model soil water vegetation types Yuanyang Terrace
DOI10.1080/10256016.2019.1601090
通讯作者Song, Weifeng(songwf85@126.com)
英文摘要The mean residence time of soil water (MRTsw) for forestland and shrubland in a water source area of Yuanyang Terrace, southwestern China, was estimated using stable isotope tracer tests and the sine-wave regression model. Stable isotope analyses from precipitation and soil water were performed in 2015. The delta H-2/delta O-18 relationship of precipitation resulted in delta H-2 = 7.31 delta O-18 + 1.49, which is nearly identical to the local meteoric water line in Kunming, southwestern, China. The MRTsw was simulated at five depth ranges (0-20, 20-40, 40-60, 60-80, 80-100 cm) of the two vegetation types by precipitation delta O-18 input data and soil water delta O-18 output data. The results showed that the MRTsw values of the forestland and shrubland both increased with soil depth. However, differences in the MRTsw of the forestland (between day 53 and 94) and of the shrubland (between day 76 and 142) were discussed. Regarding the physical properties of the soil profiles from the sample plots, non-capillary porosity decreased with soil depth in the forestland (from 48.5 to 20.5 %), and was clearly higher than that in the shrubland (from 38.8 to 18.7 %). Therefore, non-capillary porosity (macropores) could be a factor that shortens the mean residence time of soil water.
收录类别SCI
WOS关键词CATCHMENT TRANSIT-TIME ; SEASONAL-VARIATION ; FLOW ; EXTRACTION ; DELTA-O-18
WOS研究方向Chemistry ; Environmental Sciences & Ecology
WOS类目Chemistry, Inorganic & Nuclear ; Environmental Sciences
语种英语
出版者TAYLOR & FRANCIS LTD
WOS记录号WOS:000467737100003
URI标识http://www.irgrid.ac.cn/handle/1471x/2555447
专题寒区旱区环境与工程研究所
通讯作者Song, Weifeng
作者单位1.Beijing Forestry Univ, Sch Soil & Water Conservat, Beijing, Peoples R China
2.Southwest Forestry Univ, Coll Ecol & Soil & Water Conservat, Kunming, Yunnan, Peoples R China
3.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, State Key Lab Cryospher Sci, Lanzhou, Gansu, Peoples R China
4.Chinese Acad Forestry, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Ma, Jing,Song, Weifeng,Wu, Jinkui,et al. Identifying the mean residence time of soil water for different vegetation types in a water source area of the Yuanyang Terrace, southwestern China[J]. ISOTOPES IN ENVIRONMENTAL AND HEALTH STUDIES,2019,55(3):272-289.
APA Ma, Jing,Song, Weifeng,Wu, Jinkui,Liu, Zongbin,&Wei, Zheng.(2019).Identifying the mean residence time of soil water for different vegetation types in a water source area of the Yuanyang Terrace, southwestern China.ISOTOPES IN ENVIRONMENTAL AND HEALTH STUDIES,55(3),272-289.
MLA Ma, Jing,et al."Identifying the mean residence time of soil water for different vegetation types in a water source area of the Yuanyang Terrace, southwestern China".ISOTOPES IN ENVIRONMENTAL AND HEALTH STUDIES 55.3(2019):272-289.

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来源:寒区旱区环境与工程研究所

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