[Temporal and Spatial Distribution of the Soil Water <i>δ</i>D and <i>δ</i><sup>18</sup>O in a Typical Karst Valley: A Case Study of the Zhongliang Mountain, Chongqing City].
摘要
O change with soil depth gradients, which decrease along the depth in vertical direction for all types of soil land use in May but mainly increase/decrease in the cultivated land and woodland/grassland in September, respectively.
引用本文（GB/T 7714）
Wei Wu, Yongjun Jiang, Yanan Jia, 等. [Temporal and Spatial Distribution of the Soil Water <i>δ</i>D and <i>δ</i><sup>18</sup>O in a Typical Karst Valley: A Case Study of the Zhongliang Mountain, Chongqing City].[J]. PubMed, 2018.
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