soil moisture regime

The water regime of the soil is determined by the physical properties and arrangement of the soil particles. The pores in a soil determine its water-retention characteristics. When all the pores are full of water, the soil is said to be saturated. (Source: DUNSTE)



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Displaying results 1 - 9 of 9 record(s) tagged with this keywordClick/tap on any title to see full details of the record
Li B, Wang L, Kaseke KF, Li L, Seely MK 2016. The impact of rainfall on soil moisture dynamics in a foggy desert. Plos ONE 11 (10) e0164982
van Rooyen N, Bredenkamp GJ, Theron GK, Bothma J du P, Le Riche EAN 1994. Vegetational gradients around artificial watering points in the Kalahari Gemsbok National Park. Journal of Arid Environments 26 (4) 349-361
Kaseke KF, Mills AJ, Brown R, Esler KJ, Henschel JR, Seely MK 2012. A method for direct assessment of the "non rainfall" atmospheric water cycle: input and evaporation from the soil. Pure and applied geophysics 169 (5-6) 847-857
Soderberg K, Henschel J, Swap R, Macko S 2011. Environmental controls on C, N and S cycling in plants of the Namib Desert. Geophysical Research Abstracts 13
Seaquist JW, Olsson L, Ardö J 2003. A remote sensing-based primary production model for grassland biomes. Ecological Modelling 169 131-155
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