Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Kamila Báťková"'
Autor:
Kamila Báťková, Svatopluk Matula, Markéta Miháliková, Eva Hrúzová, David Kwesi Abebrese, Recep Serdar Kara, Cansu Almaz
Publikováno v:
Soil and Water Research, Vol 18, Iss 1, Pp 25-32 (2023)
The determination of the saturated hydraulic conductivity Ks on a field scale presents a challenge in which several variables have to be considered. As there is no benchmark or reference method for the Ks determination, the suitability of each availa
Externí odkaz:
https://doaj.org/article/ce6f9ac376624111979bae71b73ff711
Autor:
Kamila Báťková, Svatopluk Matula, Eva Hrúzová, Markéta Miháliková, Recep Serdar Kara, Cansu Almaz
Publikováno v:
Plant, Soil and Environment, Vol 68, Iss 7, Pp 338-346 (2022)
The study aims to indirectly determine the saturated hydraulic conductivity (Ks). The applicability of recently-published pedotransfer functions (PTFs) based on a machine learning approach has been tested, and their performance has been compared with
Externí odkaz:
https://doaj.org/article/5a625e45a08143288a4d723f6546dd1b
Autor:
Cansu Almaz, Markéta Miháliková, Kamila Báťková, Jan Vopravil, Svatopluk Matula, Tomáš Khel, Recep Serdar Kara
Publikováno v:
Hydrology, Vol 10, Iss 10, p 202 (2023)
This study introduces a simple and cost-effective method for the indirect determination of field capacity (FC) in soil, a critical parameter for soil hydrology and environmental modeling. The relationships between FC and soil moisture constants, spec
Externí odkaz:
https://doaj.org/article/db755db8522242e0845691d417d8badb
Publikováno v:
Water, Vol 15, Iss 1, p 18 (2022)
This study explores the impacts of climate change on the major components of the water balance such as surface runoff (Q), water yield (WY), and evapotranspiration (ET) in the Central Rift Valley Basin (CRVB) in Ethiopia. Projected climate data from
Externí odkaz:
https://doaj.org/article/3f977fff51844c7ca311c43b6cb4513d
Publikováno v:
Soil and Water Research, Vol 14, Iss 1, Pp 47-56 (2019)
Proper characterization of contaminants in subsurface helps to clean up effectively the contaminated sites. In this study, different methods were used to quantify non-volatile light non-aqueous phase liquid (LNAPL) and water from sample columns subje
Externí odkaz:
https://doaj.org/article/76c90768bf874f9197ec8030415432e9
Publikováno v:
Water, Vol 12, Iss 3, p 843 (2020)
Hydraulic conductivity at and near saturation (Ks and K(h)) are among the most important characteristics defining water behavior in soil. Characterization of possibilities, advantages and limitations of the Mini Disk infiltrometer (MDI) for Ks and K(
Externí odkaz:
https://doaj.org/article/2a35187f8d7c427896ffe5f176a7aa50
Autor:
Kamila BÁŤKOVÁ, Svatopluk MATULA, Markéta MIHÁLIKOVÁ, Ayele Teressa CHALA, João Manuel MOREIRA BARRADAS, Getu Bekere MEKONNEN
Publikováno v:
Soil and Water Research, Vol 9, Iss 4, Pp 161-168 (2014)
Activated carbon is a highly porous form of carbon, which has an exceptionally large surface area. Activated carbon material has been artificially processed as a set of plates, within which two different types of pores are present: micropores (< 2 nm
Externí odkaz:
https://doaj.org/article/0476baa76d8844d0bc97741cb8718f28
Publikováno v:
Türkiye Tarımsal Araştırmalar Dergisi, Vol 1, Iss 2, Pp 170-175 (2014)
Soil hydropedological data measured in situ provide an essential base for basic and also applied research in hydrological, water management, landscape and environmental disciplines. Quality of the measured data is a critical value determining the q
Externí odkaz:
https://doaj.org/article/4d585c2f491c4b1cb3d8baf8e780f997
Publikováno v:
Sensors, Vol 16, Iss 11, p 1912 (2016)
Non-destructive soil water content determination is a fundamental component for many agricultural and environmental applications. The accuracy and costs of the sensors define the measurement scheme and the ability to fit the natural heterogeneous con
Externí odkaz:
https://doaj.org/article/7dca76d60c5744088a7b727751f347ae
Publikováno v:
Journal of Soil Science and Plant Nutrition. 23:819-830