variation of soil temperature and water content of seasonal frozen soil with different vegetation coverage in the headwater region of the Yellow River, China

• Published in: Environmental earth sciences Vol. 54; no. 8; pp. 1755 - 1762
• Main Authors: Cheng, Huiyan, Wang, Genxu, Hu, Hongchang, Wang, Yibo
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Berlin/Heidelberg : Springer-Verlag 01.06.2008; Springer-Verlag; Springer; Springer Nature B.V
• Subjects: Contour chart; Earth and Environmental Science; Earth Sciences; Earth, ocean, space; Exact sciences and technology; Freshwater; Geochemistry; Geology; Marine and continental quaternary; Original Article; Rivers; Soil temperature and water content; Soils; Surficial geology; Temperature; The headwater region of the Yellow River; Vegetation; θv-T s coupling model; Huang Ho; Far East; Asia; China; China, People's Rep., Huang He R; Contour chart; θ; Soil temperature and water content; The headwater region of the Yellow River; –; coupling model; thawing; models; soil moisture; heat balance; vegetation; coupling; cyclic processes; freezing; hydrologic cycle; frozen ground; temperature; water content; soils; seasonal variations; θv-Ts coupling model
• ISSN: 0943-0105; 1866-6280; 1432-0495; 1866-6299
• DOI: 10.1007/s00254-007-0953-x

The variation and distribution of temperature and water moisture in the seasonal frozen soil is an important factor in the study of both the soil water cycle and heat balance within the source region of the Yellow River, especially under the different conditions of vegetation coverage. In this study, the impact of various degrees of vegetation coverage on soil water content and temperature was assessed. Soil moisture (θ v) and soil temperature (T s) were monitored on a daily basis. Measurements were made under different vegetation coverage (95, 70-80, 40-50 and 10%) and on both thawed and frozen soils. Contour charts of T s and θ v as well as a θ v-T s coupling model were developed in order to account for the influence of vegetation cover and the interaction between T s and θ v. It was observed that soil water content affected both the overall range and trend in the soil temperature. The regression analysis of θ v versus T s plots indicated that the soil freezing and thawing processes were significantly affected by vegetation cover changes. Vegetation coverage changes also caused variations in the θ v-T s interaction. The effect of soil water content on soil temperature during the freezing period was larger than during the thawing period. Moreover, the soil with higher vegetation coverage retained more water than that with lower coverage. In the process of freezing, the higher vegetation coverage reduced the rate of the reduction in the soil temperature because the thermal capacity of water is higher than that of soil. Areas with higher vegetation coverage also functioned better for the purpose of heat-insulating. This phenomenon may thus play an important role in the environmental protection and effective uses of frozen soil.