Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Mingyi Wen"'
Publikováno v:
Water, Vol 15, Iss 18, p 3181 (2023)
Precipitation isoscapes have provided supporting data for numerous studies of water stable isotopes, alleviating the lack of observation data. However, the applicability of simulation data from global models to specific regional contexts remains a su
Externí odkaz:
https://doaj.org/article/cb34aaddaaea44018c03b41476152f33
Publikováno v:
Agronomy, Vol 13, Iss 7, p 1711 (2023)
Understanding the dynamics of soil water and nitrate in response to typical agricultural crops in dryland ecosystems are crucial for assessing ecological consequences and informing land use planning. This study was conducted in the Changwu tableland,
Externí odkaz:
https://doaj.org/article/a493e8bdb1d541bc827acf20bc1f129a
Publikováno v:
Agronomy, Vol 13, Iss 6, p 1531 (2023)
Evapotranspiration (ET) is a crucial process in the terrestrial water cycle, and understanding its stable isotopic evolution is essential for comprehending hydrological processes. The Craig–Gordon (C-G) model is widely used to describe isotopic fra
Externí odkaz:
https://doaj.org/article/74d7957e4026480cb27396598ec6ec79
Publikováno v:
Agronomy; Volume 13; Issue 7; Pages: 1711
Understanding the dynamics of soil water and nitrate in response to typical agricultural crops in dryland ecosystems are crucial for assessing ecological consequences and informing land use planning. This study was conducted in the Changwu tableland,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=multidiscipl::8ecd9fa33495d15ddc4c1a0312aac5c9
Publikováno v:
Agronomy; Volume 13; Issue 6; Pages: 1531
Evapotranspiration (ET) is a crucial process in the terrestrial water cycle, and understanding its stable isotopic evolution is essential for comprehending hydrological processes. The Craig–Gordon (C-G) model is widely used to describe isotopic fra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=multidiscipl::25adb0be25a3f6ab7cdd8f97f449cdb9
Publikováno v:
Molecular Biotechnology.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::720edbb80770a2fcec584cc241133041
https://doi.org/10.1007/s12033-023-00754-7
https://doi.org/10.1007/s12033-023-00754-7
Publikováno v:
Hydrology and Earth System Sciences. 25:5399-5413
Soil evaporation is a key process in the water cycle and can be conveniently quantified using δ2H and δ18O in bulk surface soil water (BW). However, recent research shows that soil water in larger pores evaporates first and differs from water in sm
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::919c1fd0caab688d28b06958caf2fdb7
https://doi.org/10.5194/hess-25-5399-2021
https://doi.org/10.5194/hess-25-5399-2021
Publikováno v:
Water Resources Research. 58
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::18f2ae87905551c7bb791252a1fe1674
https://doi.org/10.1029/2022wr032182
https://doi.org/10.1029/2022wr032182
Autor:
Guangjie Chen, Wenjie Wu, Tingfang Meng, Mingyi Wen, Bingcheng Si, Jianqiang He, Min Li, Qin'ge Dong, Hao Feng, Kadambot H.M. Siddique
Publikováno v:
Journal of Hydrology. 617:128964
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::50dec120e7896e9b7197d8581e9f3f37
https://doi.org/10.1016/j.jhydrol.2022.128964
https://doi.org/10.1016/j.jhydrol.2022.128964
Publikováno v:
Hydrological Processes. 35
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f2310dec1301d4dff628254658548bc9
https://doi.org/10.1002/hyp.14248
https://doi.org/10.1002/hyp.14248