Zobrazeno 1 - 10
of 75
pro vyhledávání: '"Victor F Bense"'
Autor:
Aaron A Mohammed, Julia A Guimond, Victor F Bense, Rob C Jamieson, Jeffrey M McKenzie, Barret L Kurylyk
Publikováno v:
Environmental Research Letters, Vol 17, Iss 12, p 124036 (2022)
Permafrost thaw leads to an increase in groundwater circulation and potential mobilization of organic carbon sequestered in deep Arctic sediments (e.g. 3–25 m below surface). Upon thaw, a portion of this carbon may be transported along new groundwa
Externí odkaz:
https://doaj.org/article/dde8ea021dc14d7685630f04c1437715
Publikováno v:
Environmental Research Letters, Vol 17, Iss 4, p 045027 (2022)
Groundwater discharge is an important mechanism through which fresh water and associated solutes are delivered to the ocean. Permafrost environments have traditionally been considered hydrogeologically inactive, yet with accelerated climate change an
Externí odkaz:
https://doaj.org/article/77dda524b8864395a2157d293b745d83
Autor:
Qing-Feng Wang, Hui-Jun Jin, Dong-Liang Luo, Yu Sheng, Jun Wen, Chien-Lu Ping, Mark H. Clark, Qiang Ma, Xiao-Ying Jin, Ji-Chun Wu, Yu-Zhong Yang, Qiang Li, Raul D. Şerban, Daqing Yang, Victor F. Bense, Qing-Bai Wu
Publikováno v:
Advances in Climate Change Research, Vol 15, Iss 5, Pp 830-844 (2024)
Ground freeze‒thaw processes have significant impacts on infiltration, runoff and evapotranspiration. However, there are still critical knowledge gaps in understanding of hydrological processes in permafrost regions, especially of the interactions
Externí odkaz:
https://doaj.org/article/431e9b6a81b14baf8c04c67d50296daf
Autor:
Qiang MA, Hui-Jun JIN, Victor F. BENSE, Dong-Liang LUO, Sergey S. MARCHENKO, Stuart A. HARRIS, Yong-Chao LAN
Publikováno v:
Advances in Climate Change Research, Vol 10, Iss 4, Pp 225-239 (2019)
Many observations in and model simulations for northern basins have confirmed an increased streamflow from degrading permafrost, while the streamflow has declined in the source area of the Yellow River (SAYR, above the Tanag hydrological station) on
Externí odkaz:
https://doaj.org/article/4a0150039644467ab73c683cd7fe8e50
Autor:
Sjoukje Irene de Lange, Dhruv Sehgal, Núria Martínez-Carreras, Kryss Waldschläger, Victor F. Bense, Christophe Hissler, A.J.F. (Ton) Hoitink
Accurate particle size distribution (PSD) measurements of suspended particulate matter composed of flocs and aggregates are important to improve understanding of ecological and geomorphological processes, and for environmental engineering application
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::29f3edcbfb0ce3004ede0d0d02153c3f
https://doi.org/10.22541/essoar.168319822.29525394/v1
https://doi.org/10.22541/essoar.168319822.29525394/v1
Publikováno v:
Vadose Zone Journal 22 (2023) 3
Permafrost regions are experiencing increasing air temperatures, accelerating the thawing process, and thickening the active layer in summer. This can accelerate the release of greenhouse gasses into the atmosphere from the organic carbon stored in t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::28cac904aa22b38d9701eadd14072212
https://research.wur.nl/en/publications/soil-thermal-properties-during-freezethaw-dynamics-as-function-of
https://research.wur.nl/en/publications/soil-thermal-properties-during-freezethaw-dynamics-as-function-of
Publikováno v:
Hydrogeology Journal, 30(4), 1233-1257. Springer Heidelberg
Lapperre, R E, Bense, V F, Kasse, C & van Balen, R 2022, ' Temporal and spatial variability of cross-fault groundwater level differences: the impact of fault-induced permeability reduction, precipitation and evapotranspiration ', Hydrogeology Journal, vol. 30, no. 4, pp. 1233-1257 . https://doi.org/10.1007/s10040-022-02465-w
Lapperre, R E, Bense, V F, Kasse, C & van Balen, R 2022, ' Temporal and spatial variability of cross-fault groundwater level differences: the impact of fault-induced permeability reduction, precipitation and evapotranspiration ', Hydrogeology Journal, vol. 30, no. 4, pp. 1233-1257 . https://doi.org/10.1007/s10040-022-02465-w
Faults in the Roer Valley Rift System (Netherlands, Belgium, and Germany) act as barriers to lateral groundwater flow in unconsolidated sedimentary aquifers. This causes a cross-fault groundwater-level step of up to several metres. Using a dataset ob
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b26014fc35e0fea18ae651e803d5d68e
https://research.vu.nl/en/publications/0efabb6a-da72-47b9-a2b7-5df936dec83b
https://research.vu.nl/en/publications/0efabb6a-da72-47b9-a2b7-5df936dec83b
Publikováno v:
Hydrogeology Journal. 28:1787-1807
Managed aquifer recharge (MAR) is a strategy to address dwindling water availability that is used to recharge stressed groundwater systems for recovery or adaptation purposes. Glacial moraine complexes can host large groundwater volumes in thick coar
Autor:
Dhruv Sehgal, Núria Martínez‐Carreras, Christophe Hissler, Victor F. Bense, A. J. F. (Ton) Hoitink
Publikováno v:
Journal of Geophysical Research: Earth Surface 127 (2022) 12
Journal of Geophysical Research: Earth Surface, 127(12)
Journal of Geophysical Research: Earth Surface, 127(12)
Optical turbidity sensors have become standard instrumentation to estimate suspended particulate matter concentration (SPMC). However, turbidity readings respond to factors other than SPMC, such as particle size and shape, organic fraction, sediment
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3fb74b4133927e7bcbbac481c0138c0c
https://research.wur.nl/en/publications/a-generic-relation-between-turbidity-suspended-particulate-matter
https://research.wur.nl/en/publications/a-generic-relation-between-turbidity-suspended-particulate-matter
Autor:
Victor F. Bense, Dongliang Luo, Yong-Chao Lan, Sergey Marchenko, Stuart A. Harris, Huijun Jin, Qiang Ma
Publikováno v:
Advances in Climate Change Research 10 (2019) 4
Advances in Climate Change Research, 10(4), 225-239
Advances in Climate Change Research, Vol 10, Iss 4, Pp 225-239 (2019)
Advances in Climate Change Research, 10(4), 225-239
Advances in Climate Change Research, Vol 10, Iss 4, Pp 225-239 (2019)
Many observations in and model simulations for northern basins have confirmed an increased streamflow from degrading permafrost, while the streamflow has declined in the source area of the Yellow River (SAYR, above the Tanag hydrological station) on