In the Netherlands, water-repellent soils are widespread and they often show irregular moisture patterns, which cause accelerated transport of water and solutes to the groundwater and surface water. Under grass cover, spatial variability in soil moisture content is high owing to fingered flow; in arable land, vegetation and microtopography play a dominant role. Examples are given of uneven soil moisture patterns in water-repellent sandy, loam, clay and peat soils with grass cover, and in cropped water-repellent sandy soils. In addition, the influence of fungi on inducing soil moisture patterns is illustrated as well
Knowledge of soil water repellency distribution, of factors affecting its occurrence and of its hydr...
Water repellency (hydrophobicity) is known to be temporally variable. Most studies indicate that soi...
Knowledge of soil water repellency distribution, of factors affecting its occurrence and of its hydr...
In the Netherlands, water-repellent soils are widespread and they often show irregular moisture patt...
Various factors contribute to the spatial variation of the soil water content and solute concentrati...
The present study suggests that many soils in the Netherlands, in natural as well as in agricultural...
The present study suggests that many soils in the Netherlands, in natural as well as in agricultural...
The variation in water content of grass-covered peaty clay and clayey peat soils was studied at six ...
The variation in water content of grass-covered peaty clay and clayey peat soils was studied at six ...
Man-made raised sandy soils in the Netherlands are classified as `brown' or `black' plaggen soils. W...
Man-made raised sandy soils in the Netherlands are classified as `brown' or `black' plaggen soils. W...
Man-made raised sandy soils in the Netherlands are classified as `brown' or `black' plaggen soils. W...
In soils with fingered flow, surface-applied solutes can reach the groundwater more rapidly than in ...
Grass-covered heavy basin clay soils in the Netherlands appeared to be water-repellent. Water-repell...
Grass-covered heavy basin clay soils in the Netherlands appeared to be water-repellent. Water-repell...
Knowledge of soil water repellency distribution, of factors affecting its occurrence and of its hydr...
Water repellency (hydrophobicity) is known to be temporally variable. Most studies indicate that soi...
Knowledge of soil water repellency distribution, of factors affecting its occurrence and of its hydr...
In the Netherlands, water-repellent soils are widespread and they often show irregular moisture patt...
Various factors contribute to the spatial variation of the soil water content and solute concentrati...
The present study suggests that many soils in the Netherlands, in natural as well as in agricultural...
The present study suggests that many soils in the Netherlands, in natural as well as in agricultural...
The variation in water content of grass-covered peaty clay and clayey peat soils was studied at six ...
The variation in water content of grass-covered peaty clay and clayey peat soils was studied at six ...
Man-made raised sandy soils in the Netherlands are classified as `brown' or `black' plaggen soils. W...
Man-made raised sandy soils in the Netherlands are classified as `brown' or `black' plaggen soils. W...
Man-made raised sandy soils in the Netherlands are classified as `brown' or `black' plaggen soils. W...
In soils with fingered flow, surface-applied solutes can reach the groundwater more rapidly than in ...
Grass-covered heavy basin clay soils in the Netherlands appeared to be water-repellent. Water-repell...
Grass-covered heavy basin clay soils in the Netherlands appeared to be water-repellent. Water-repell...
Knowledge of soil water repellency distribution, of factors affecting its occurrence and of its hydr...
Water repellency (hydrophobicity) is known to be temporally variable. Most studies indicate that soi...
Knowledge of soil water repellency distribution, of factors affecting its occurrence and of its hydr...