Transference of Robinia pseudoacacia water-use patterns from deep to shallow soil layers during the transition period between the dry and rainy seasons in a water-limited region

• Published in: Forest ecology and management 2020-02, Vol.457, p.117727, Article 117727
• Main Authors: Zhao, Yali, Wang, Yunqiang, He, Meina, Tong, Yongping, Zhou, Jingxiong, Guo, Xiangyu, Liu, Jinzhao, Zhang, Xingchang
• Format: Article
• Language: English
• Subjects: Dried soil layer; Robinia pseudoacacia; Stable isotopes; The Loess Plateau; Water uptake pattern
• ISSN: 0378-1127; 1872-7042
• DOI: 10.1016/j.foreco.2019.117727

•Stable isotopes and root distributions were used to identify water uptake of R. pseudoacacia.•The water-use pattern of R. pseudoacacia exhibited variation during the transition period.•The percentage of water used in shallow soil layers increased from April to July.•Water uptake from the deep soil layers decreased from April to July.•Water-use patterns during the dry season can aggravate the development of dry soil layers. Soil water plays a critical role in determining plant survival and growth globally, especially in water-limited regions. This study explores water-use characteristics of Robinia pseudoacacia during the transition period between the dry and rainy seasons in the Chinese Loess Plateau (CLP). A stable isotope technique (δ18O and δD) and two complementary approaches (i.e., the direct inference method and the MixSIAR model) were used to distinguish water source changes during this transition period. Based on δ18O and δD distribution patterns, we subdivided a 500 cm soil profile into four potential water sources: shallow (0–40 cm), intermediate-shallow (40–120 cm), intermediate (120–200 cm) and deep (200–500 cm). During the transition period, R. pseudoacacia exhibited different water uptake patterns. In April 26.2% and 48.4% of water uptake derived from the 40 to 120 and 200 to 500 cm soil profile layers; in May, 21.5%, 24.5% and 37.4% of water was absorbed from the 0 to 40, 40 to 120 and 200 to 500 cm soil profile layers. In June and July, 51.6% and 53.6% of the water mainly derived from the 0 to 120 cm soil profile layer, respectively. During the dry season (April), the trend in water uptake shifted to the deep soil layer, potentially a key period for the onset of soil desiccation in this soil layer. As precipitation increased, the proportion of water uptake from the shallow and intermediate-shallow soil layers increased. Because water-use pattern characteristics could provide important information on the development of the dried soil layer (DSL), the stable isotope technique could help reveal the water sources used by trees while also offering insight into water movement mechanisms of local ecosystems. Given its usefulness, the application of the stable isotope technique should be expanded in analyzing practical ecohydrological issues that occur in deep soils in the future.