Zobrazeno 1 - 10
of 56
pro vyhledávání: '"Klaas Metselaar"'
Autor:
Murilo dos Santos Vianna, Klaas Metselaar, Quirijn de Jong van Lier, Thomas Gaiser, Fábio Ricardo Marin
Publikováno v:
Agricultural Water Management, Vol 301, Iss , Pp 108938- (2024)
Process-based crop models have faced rapid development over the last years, and many modelling platforms are now available and can be used in a wide range of conditions. Whilst the selection of a model should be suited to the purpose of its applicati
Externí odkaz:
https://doaj.org/article/50bb75016eee41cfbe276e2eae687795
Autor:
Klaas Metselaar
Publikováno v:
Journal of Hydrology X, Vol 19, Iss , Pp 100151- (2023)
The NCRS-curve number equation allows calculating the storm runoff from a rainfall event for specific types of land use. It was based on an analysis of direct runoff data using baseflow corrected hydrographs and rainfall. Given this basis, the curve
Externí odkaz:
https://doaj.org/article/88eb8c9595d94880bedfc8b84fe01d18
Publikováno v:
MethodsX, Vol 4, Iss C, Pp 134-142 (2017)
The saturated hydraulic conductivity (Ks) is a key characteristic of porous media, describing the rate of water flow through saturated porous media. It is an indispensable parameter in a broad range of simulation models that quantify saturated and/or
Externí odkaz:
https://doaj.org/article/b7513fed03294c5183d79e2b343af9dd
Publikováno v:
Vadose Zone Journal, Vol 17, Iss 1 (2018)
Predicting soil water availability to plants is important for agricultural and ecological models. Models that explicitly take into account root water uptake and transpiration reduction describe the ability of soil to supply water to plants based on s
Externí odkaz:
https://doaj.org/article/a8a9fdf8928d4738a1483609841f89eb
Publikováno v:
Soil Systems, Vol 3, Iss 3, p 44 (2019)
The geometry of rooting systems is important for modeling water flows in the soil-plant-atmosphere continuum. Measured information about root density can be summarized in adjustable equations applied in hydrological models. We present such descriptiv
Externí odkaz:
https://doaj.org/article/0649bb3bfa88406bba22bb6f482d60df
Publikováno v:
Agronomy, Vol 9, Iss 3, p 160 (2019)
The effects of water stress on crop yield through modifications of plant architecture are vital to crop performance such as common bean plants. To assess the extent of this effect, an outdoor experiment was conducted in which common bean plants recei
Externí odkaz:
https://doaj.org/article/4e9960de379a45db9fbd1d3b8594c314
Autor:
Durval Dourado-Neto, Quirijn de Jong van Lier, Klaas Metselaar, Klaus Reichardt, Donald R. Nielsen
Publikováno v:
Scientia Agricola, Vol 67, Iss 1, Pp 87-95 (2010)
The original Thornthwaite and Mather method, proposed in 1955 to calculate a climatic monthly cyclic soil water balance, is frequently used as an iterative procedure due to its low input requirements and coherent estimates of water balance components
Externí odkaz:
https://doaj.org/article/70677946559b471a9c3d3e529bad6452
Publikováno v:
Water resources research, 57(8):e2020WR028286, 1-14. Wiley-Blackwell
Water Resources Research 57 (2021) 8
Water Resources Research, 57(8)
Water Resources Research 57 (2021) 8
Water Resources Research, 57(8)
Modeling of water vapor transport through a dry soil layer (DSL), typically formed in the top soil during dry seasons in arid and semi-arid areas, is still problematic. Previous laboratory experiments in controlled environments showed that the only v
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b830b1e5421297742238c9ae58380500
https://doi.org/10.1029/2020wr028286
https://doi.org/10.1029/2020wr028286
Publikováno v:
MethodsX
MethodsX, 4, 134-142
MethodsX 4 (2017)
MethodsX, Vol 4, Iss C, Pp 134-142 (2017)
MethodsX, 4, 134-142
MethodsX 4 (2017)
MethodsX, Vol 4, Iss C, Pp 134-142 (2017)
Graphical abstract
The saturated hydraulic conductivity (Ks) is a key characteristic of porous media, describing the rate of water flow through saturated porous media. It is an indispensable parameter in a broad range of simulation models that q
The saturated hydraulic conductivity (Ks) is a key characteristic of porous media, describing the rate of water flow through saturated porous media. It is an indispensable parameter in a broad range of simulation models that q
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d638ce6a184d670e140e09b4b313eb37
http://europepmc.org/articles/PMC5345952
http://europepmc.org/articles/PMC5345952
Autor:
Alain Francés, L. Reyes-Acosta, E. Balugani, C. van der Tol, Klaas Metselaar, Maciek W. Lubczynski
Publikováno v:
Journal of hydrology, 547, 54-66. Elsevier
Journal of Hydrology 547 (2017)
Journal of Hydrology, 547, 54-66
Journal of Hydrology 547 (2017)
Journal of Hydrology, 547, 54-66
Studies on evapotranspiration partitioning under eddy covariance (EC) towers rarely address the separate effects of transpiration and evaporation on groundwater resources. Such partitioning is important to accurately assess groundwater resources, esp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4cf489351a24e494f5dc5cc53c093ae9
https://doi.org/10.1016/j.jhydrol.2017.01.042
https://doi.org/10.1016/j.jhydrol.2017.01.042