Effect of Soil Moisture Content on Condensation Water in Typical Loess and Sandy Soil DOI Creative Commons
Jin Cheng,

Zhifeng Jia,

Li Ge

et al.

Land, Journal Year: 2024, Volume and Issue: 13(7), P. 934 - 934

Published: June 27, 2024

Many scholars have used samples of drying soil to observe the amount condensation water, which may exaggerated regional as water content in natural state was not considered. To analyze effect moisture on state, volume loess and sandy under different gravimetric conditions measured autumn 2022 spring 2023 using micro-lysimeters combined with weighing method at groundwater environment site Chang’an University, Guanzhong Basin, China. The results showed that average daily 0%, 3%, 7%, 11%, 15% 0.34, 0.09, 0.01, −0.05, −0.07 mm days 54, 40, 24, 21, 16, respectively, 0.21, −0.02, −0.28, −0.82, −1.35 2, 3, 1, respectively. Under same conditions, had more than soil. Soil occurred mainly when less it negatively correlated content. quantity positively relative humidity air temperature–dew point differences. Relative exceeding 60% differences below 8 °C were favorable for formation water. This study provides a reference assessment state.

Language: Английский

Effect of Soil Moisture Content on Condensation Water in Typical Loess and Sandy Soil DOI Creative Commons
Jin Cheng,

Zhifeng Jia,

Li Ge

et al.

Land, Journal Year: 2024, Volume and Issue: 13(7), P. 934 - 934

Published: June 27, 2024

Many scholars have used samples of drying soil to observe the amount condensation water, which may exaggerated regional as water content in natural state was not considered. To analyze effect moisture on state, volume loess and sandy under different gravimetric conditions measured autumn 2022 spring 2023 using micro-lysimeters combined with weighing method at groundwater environment site Chang’an University, Guanzhong Basin, China. The results showed that average daily 0%, 3%, 7%, 11%, 15% 0.34, 0.09, 0.01, −0.05, −0.07 mm days 54, 40, 24, 21, 16, respectively, 0.21, −0.02, −0.28, −0.82, −1.35 2, 3, 1, respectively. Under same conditions, had more than soil. Soil occurred mainly when less it negatively correlated content. quantity positively relative humidity air temperature–dew point differences. Relative exceeding 60% differences below 8 °C were favorable for formation water. This study provides a reference assessment state.

Language: Английский

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