Zobrazeno 1 - 10
of 22
pro vyhledávání: '"Kuandi Zhang"'
Publikováno v:
Journal of Water Supply: Research and Technology-Aqua.
To determine the response between the onshore sediment transport capacity (Tc) and various hydraulic parameters, a variable-slope, fixed-bed flume experiment was conducted to investigate Tc for five slopes and six flow rates by comparing five levels
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e14edd3f68ffa54b3a1b09730167ac57
https://doi.org/10.2166/aqua.2022.054
https://doi.org/10.2166/aqua.2022.054
Publikováno v:
Hydrological Processes. 36
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2b02f47eea0e29457edff646d2c86215
https://doi.org/10.1002/hyp.14707
https://doi.org/10.1002/hyp.14707
Publikováno v:
Hydrological Processes. 36
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8874e45f1ea85879915f204636ab7526
https://doi.org/10.1002/hyp.14705
https://doi.org/10.1002/hyp.14705
Publikováno v:
CATENA. 223:106929
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fef14a349ac5788c0899fc65413ffde9
https://doi.org/10.1016/j.catena.2023.106929
https://doi.org/10.1016/j.catena.2023.106929
Publikováno v:
Journal of Soils and Sediments. 20:2289-2305
Sediment transport plays a vital role in the development of soil erosion process models. The primary purpose of this study is to establish new sediment transport capacity formulas and evaluate their applicability to sediment. In this study, we collec
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4370a7e394b7c5c74061eb6e20365547
https://doi.org/10.1007/s11368-020-02568-5
https://doi.org/10.1007/s11368-020-02568-5
Publikováno v:
Geoderma. 429:116264
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::adaa3627c93ed402fff58d203e70e4d5
https://doi.org/10.1016/j.geoderma.2022.116264
https://doi.org/10.1016/j.geoderma.2022.116264
Publikováno v:
Hydrological Processes. 35
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::edcd3aa55f28f7bad1f29588bd180a9e
https://doi.org/10.1002/hyp.14408
https://doi.org/10.1002/hyp.14408
Publikováno v:
CATENA. 218:106576
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc7c5dd813a9a22b4119450d00688820
https://doi.org/10.1016/j.catena.2022.106576
https://doi.org/10.1016/j.catena.2022.106576
Publikováno v:
Hydrological Processes. 34:823-835
Soil erosion is a major contributor to land degradation in the Loess Plateau in China. To clarify the sediment transport capacity of overland flow influenced by hydraulic parameters, such as shear stress, sand shear stress (hydraulic gradient partiti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b6370724a63f2664447692ecd83c7d1c
https://doi.org/10.1002/hyp.13634
https://doi.org/10.1002/hyp.13634
Publikováno v:
Hydrology Research. 50:1324-1343
Overland flow is the initial driver of slope surface erosion. To discover resistance characteristics of overland flow influenced by rainfall intensity and roughness, indoor simulated rainfall experiments with six kinds of roughness, five flow dischar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::beffc37f72d6c958e51dae9866807eea
https://doi.org/10.2166/nh.2019.261
https://doi.org/10.2166/nh.2019.261