Dynamics of soil water, temperature, and salt and their coupled effects in Haloxylon ammodendron forests of different ages in an arid desert oasis ecotone

• Published in: Journal of Hydrology: Regional Studies
• Main Authors: Changsheng Shen, Guohua Wang, Qianqian Gou
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier 2024
• Subjects: Typical desert–oasis ecotone; Haloxylon ammodendron; Seasonal permafrost; Soil water and salt migration; Synergetic variations; Physical geography; GB3-5030; Geology; QE1-996.5; permafrost
• Online Access: https://doi.org/10.1016/j.ejrh.2024.101965; https://doaj.org/article/cb788c7f928241e589ffc6d7305288c2

Study region: The study region is a typical desert oasis ecotone of the Hexi Corridor, Northwest China. Study focus: Based on four years of in situ observational data of soil water, temperature, and electrical conductivity obtained from three Haloxylon ammodendron (H. ammodendron) forests (20, 30 and 50 years) in a typical desert oasis ecotone (DOE) of the Hexi Corridor, in this study, the mechanisms of change and coupled effects of water, heat, and salt in frozen desert soils along a long-term shrub plantation in a typical desert oasis ecotone are presented. New hydrological insights for the region: This study revealed that changes in soil water, heat, and salt and their coupling effects were completely different between shallow (0–80 cm) and deep (160–200 cm) depths. At 0–80 cm, soil water gradually decreased in the 50-year-old H. ammodendron plot, but soil salt first increased in the 30-year plot and then decreased in the 50-year plot. When the freezing process occurred in the 0–80 cm depth interval, the soil water and salt contents decreased nonlinearly with the absolute value of the soil temperature (|T|), following a power function and logarithmic function, respectively. For the thawing process in the 0–80 cm depth interval, soil water and salt increased with increasing temperature, and there was a significant linear relationship between soil water and salt (P<0.01). In the 160–200 cm layer, soil water and salt significantly increased after 30–50 years during the growing season.