Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Yi Zhih Tsai"'
Publikováno v:
Land, Vol 11, Iss 9, p 1518 (2022)
When surface water infiltrates soil, the fine soil particles carried in water gradually clog soil pores and form a low-permeability soil layer. Clogging impacts the variations in pore water pressure heads in soil and effective hydraulic conductivity.
Externí odkaz:
https://doaj.org/article/c9e8036b16864c748e1162d5dc78aebc
Publikováno v:
Groundwater. 61:203-214
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2c4094ce6db8f24d2bef6c6f4eb9719f
https://doi.org/10.1111/gwat.13295
https://doi.org/10.1111/gwat.13295
Autor:
Yi-Zhih Tsai, Kan-Sheng Hsu, Hung-Yu Wu, Shu-I Lin, Hwa-Lung Yu, Kuo-Tsang Huang, Ming-Che Hu, Shao-Yiu Hsu
Publikováno v:
Water, Vol 12, Iss 4, p 1176 (2020)
Climate change might potentially cause extreme weather events to become more frequent and intense. It could also enhance water scarcity and reduce food security. More efficient water management techniques are thus required to ensure a stable food sup
Externí odkaz:
https://doaj.org/article/a49ebeafdd5f4ef7bab00d93b96aacba
Publikováno v:
Geofluids, Vol 2018 (2018)
Darcy-scale capillary pressure is traditionally assumed to be constant. By contrast, a considerable gap exists between the measured and equilibrium capillary pressures when the same moisture saturation is considered with a high flow rate, and this ga
Externí odkaz:
https://doaj.org/article/5b284e9963ed461f9bf04d4f570f8930
Publikováno v:
Journal of Hydrology. 621:129524
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a969508bee45885444425d85faa8d67a
https://doi.org/10.1016/j.jhydrol.2023.129524
https://doi.org/10.1016/j.jhydrol.2023.129524
Autor:
Kan-Sheng Hsu, Ming-Che Hu, Kuo-Tsang Huang, Hwa-Lung Yu, Hung-Yu Wu, Shao Yiu Hsu, Shu-I. Lin, Yi-Zhih Tsai
Publikováno v:
Water
Volume 12
Issue 4
Water, Vol 12, Iss 1176, p 1176 (2020)
Volume 12
Issue 4
Water, Vol 12, Iss 1176, p 1176 (2020)
Climate change might potentially cause extreme weather events to become more frequent and intense. It could also enhance water scarcity and reduce food security. More efficient water management techniques are thus required to ensure a stable food sup
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d8faf84810fc0c64ef362d6aaaebe7a7
Autor:
Jung-Dung Lee, Yung-Chia Chiu, Yi-Zhih Tsai, Tsung Yu Lee, Shao Yiu Hsu, Hung-Yen Lin, Jui-Hsiang Lo
Studies have indicated that the streambed with the clogging layer affects the interaction between surface water and groundwater. When the streambed covered by a clogging layer, the decrease of the groundwater table can transform the state of stream-g
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b484386c9a2fc38f8b307d62e0b76b1b
https://doi.org/10.5194/egusphere-egu2020-14976
https://doi.org/10.5194/egusphere-egu2020-14976
Publikováno v:
Journal of Hydrology. 582:124445
In recent years, more studies have been focusing on the transient behaviors of the movement of soil water and changes in matric potential, which require the measurement of the rapid changes in matric potential or capillary pressure. Because of the de
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2e0a7cf02e51eabbada6cbef1e64cc63
https://doi.org/10.1016/j.jhydrol.2019.124445
https://doi.org/10.1016/j.jhydrol.2019.124445
Publikováno v:
Geofluids, Vol 2018 (2018)
Darcy-scale capillary pressure is traditionally assumed to be constant. By contrast, a considerable gap exists between the measured and equilibrium capillary pressures when the same moisture saturation is considered with a high flow rate, and this ga
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6d9d3e34376462fa04bf386e3aa28354
https://doaj.org/article/5b284e9963ed461f9bf04d4f570f8930
https://doaj.org/article/5b284e9963ed461f9bf04d4f570f8930
Autor:
Yi-Zhih Tsai, 蔡義誌
96
There is inseparable relation between moisture movement in soil and pore size distribution of porous media. Therefore, this study developed two one-dimensional vertical flow hydraulic conductivity functions which are based on Arya and Kosugi
There is inseparable relation between moisture movement in soil and pore size distribution of porous media. Therefore, this study developed two one-dimensional vertical flow hydraulic conductivity functions which are based on Arya and Kosugi
Externí odkaz:
http://ndltd.ncl.edu.tw/handle/50356891806110181225