The temporal variation in a soil moisture profile can be studied using resistivity sounding data acquired at different times. The layered earth model based estimation of soil moisture from apparent resistivity data is a two-step non-linear inversion. Firstly, the apparent resistivity data are invert
Estimation of actual evaporation using precipitation and soil moisture records in arid climates
β Scribed by A. U. Sorman; M. J. Abdulrazzak
- Publisher
- John Wiley and Sons
- Year
- 1995
- Tongue
- English
- Weight
- 949 KB
- Volume
- 9
- Category
- Article
- ISSN
- 0885-6087
No coin nor oath required. For personal study only.
β¦ Synopsis
There is little knowledge available about infiltration and evaporation processes in wadi channels in arid regions. This work was conducted to determine the actual evaporation from bare soils in wadi channels in the south-western region of the Kingdom of Saudi Arabia. The estimation of soil evaporation is highly dependent on the availability of moisture in the upper layers of alluvial wadis, in which the areal rainfall, flood hydrograph and soil properties play a significant part.
The study was conducted by estimating the actual evaporation using soil moisture data. precipitation and runoff depths in a representative basin. The results are compared with potential rates. The actual rates were 1.5 mm/day immediately after a rainy day and then decreased to 0,42mm/day. The minimum rate was about 0.1-0.2mm/day during the dry season. The potential rates were about 9.5 mm/day in June and July, decreasing to 3 5 mm/day in December and January.
π SIMILAR VOLUMES
## Abstract Soil salinity is one of the great problems in arid and semiβarid environments. The estimation and prediction of spatial soil salinity may be considered as a stochastic process, observed at irregular locations in space. Environmental variables usually show spatial dependence among observ
## Abstract The Soil Conservation Service curve number (CN) method commonly uses three discrete levels of soil antecedent moisture condition (AMC), defined by the 5βday antecedent rainfall depth, to describe soil moisture prior to a runoff event. However, this way may not adequately represent soil