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- W2073405496 abstract "Abstract The soil water regime is a key component of the current UK land evaluation systems. However, direct quantification requires many years of measurements which are not available for large parts of the country. One method for extending existing data is through the use of soil water simulation models. A physically based, one-dimensional soil water simulation model (SOIL) was calibrated against relatively easily obtained dipwell, soil water retention and saturated hydraulic conductivity data for eight relatively level sites in Scotland with limited potential for lateral flow. However, the calibration was only possible through the use of an inverse modelling procedure to select a matric potential which gave a `best-fit' to the appearance of saturated conditions in the dipwells. The calibrated model was subsequently able to accurately predict the fluctuations in the perched watertable to within one depth class in five soil profiles and only slightly greater than one depth class in the remainder. The technique offers the potential to extrapolate from a limited period of measured soil watertable data. However, care is needed as there were additional errors associated with the restrictions imposed by the model, by the input data and due to the nature of the calibration data." @default.
- W2073405496 created "2016-06-24" @default.
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- W2073405496 date "1999-07-01" @default.
- W2073405496 modified "2023-09-25" @default.
- W2073405496 title "The use of inverse modelling and dipwell data in the calibration and evaluation of a soil water simulation model" @default.
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- W2073405496 doi "https://doi.org/10.1016/s0016-7061(98)00120-7" @default.
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