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  • New
  • Open Access Icon
  • Research Article
  • 10.17221/106/2025-swr
Ca-Mg-Al LDH-modified wheat straw biochar for efficient lead chemisorption from aqueous solution: Insights from isotherm and kinetic analyses
  • Jan 20, 2026
  • Soil and Water Research
  • Muhammad Tahir Amin + 4 more

  • Open Access Icon
  • Research Article
  • 10.17221/91/2025-swr
The response of medium and trace elements in degraded alpine meadow soils to vegetation characteristics and soil physicochemical properties
  • Jan 4, 2026
  • Soil and Water Research
  • Haowei Xu + 3 more

  • Open Access Icon
  • Research Article
  • 10.17221/39/2025-swr
Rainfall pattern impact on runoff and sediment of the sloping cropland in Northeast China
  • Jan 4, 2026
  • Soil and Water Research
  • Xu Fan + 5 more

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  • Research Article
  • 10.17221/47/2025-swr
Multi-objective optimisation and synergistic mechanisms of expansive soil improvement using organic fertiliser, slow-release fertiliser, and rice straw
  • Jan 4, 2026
  • Soil and Water Research
  • Yonggang Huang + 5 more

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  • Research Article
  • 10.17221/33/2025-swr
Economic evaluation of conservation grassland as a measure to control soil erosion in the Czech Republic
  • Oct 3, 2025
  • Soil and Water Research
  • Ivo Horák + 6 more

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  • Research Article
  • 10.17221/24/2025-swr
The role of ground heat flux in estimating evapotranspiration by the Penman-Monteith method on mountain meadow
  • Oct 1, 2025
  • Soil and Water Research
  • Michal Dohnal + 3 more

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  • Research Article
  • 10.17221/22/2025-swr
Determination of soil loss on agricultural land based on field measurements in the Czech Republic
  • Sep 30, 2025
  • Soil and Water Research
  • Jiří Kapička + 6 more

The current erosion protection set up in the Czech Republic (CZ) is based on the long-term soil loss due to water erosion using the Universal Soil Loss Equation (USLE). The range of recommended values of tolerable soil loss by water varies among different authors and approaches, depending on the specific area and its parameters. It is, therefore, important to ask the following questions. What is the real range of soil loss by water erosion in CZ. To determine the range of soil loss, a model extrapolation was carried out. The model extrapolation was based on the results from two main experimental measurements. Both from the evaluated volume soil loss of real erosion events and field experiments based on measurements of erosion induced by artificial rainfall. The results of modelled extrapolation of the range of long-term soil loss are in the range 6.9-13.8 t/ha per year.

  • Open Access Icon
  • Research Article
  • 10.17221/25/2025-swr
Alternative solution for determining the irrigation water quantity: ET<sub>Gauge</sub>
  • Jul 18, 2025
  • Soil and Water Research
  • Ismail Tas + 1 more

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  • Research Article
  • 10.17221/56/2025-swr
Rainfall induced changes in soil moisture: A comparative study of conventional and strip tillage
  • Jul 4, 2025
  • Soil and Water Research
  • Vojtěch Štros + 3 more

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  • Research Article
  • 10.17221/28/2025-swr
Effects of variable rate fertiliser application on selected macronutrients leaching from the ploughed layer
  • Jul 1, 2025
  • Soil and Water Research
  • Jan Vopravil + 4 more