1992
DOI: 10.2172/5593126
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A modeling study of water flow in the vadose zone beneath the Radioactive Waste Management Complex

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Cited by 8 publications
(21 citation statements)
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“…Hydrologic properties for the sedimentary lithologic units were derived primarily from site‐specific characterization and inverse modeling studies (McElroy and Hubbell, 1990; Baca et al, 1992; Bhorgese, 1988; Martian, 1995; Magnuson, 1995). Table 1 shows the assigned homogenous properties for the surficial sediment and the AB interbed.…”
Section: Base Model Developmentmentioning
confidence: 99%
See 1 more Smart Citation
“…Hydrologic properties for the sedimentary lithologic units were derived primarily from site‐specific characterization and inverse modeling studies (McElroy and Hubbell, 1990; Baca et al, 1992; Bhorgese, 1988; Martian, 1995; Magnuson, 1995). Table 1 shows the assigned homogenous properties for the surficial sediment and the AB interbed.…”
Section: Base Model Developmentmentioning
confidence: 99%
“…The parameters for the van Genuchten constitutive equations for all the sediments in the model were α = 1.066 m −1 , β = 1.523, and S wr = 0.142. These values were obtained from averaging the results of characterization activities on core samples from the surficial sediments (Baca et al, 1992).…”
Section: Base Model Developmentmentioning
confidence: 99%
“…A summary of several important modeling investigations is presented below. Baca et al (1992) used several analytical hydrological models to simulate infiltration rates, evaluate the effects of past flooding events on pit 10, and estimate water travel times in the vadose zone. Input parameters to the models included climatic data (specifically for the infiltration calculations), unsaturated hydraulic properties (including representative characteristic curves and hydraulic conductivity curves), and saturated hydraulic parameters such as hydraulic conductivity and effective porosity.…”
Section: 73mentioning
confidence: 99%
“…Specifically, the code has the ability to account for (a) liquid and vapor water movement, (b) heat transfer by conduction and convection, (c) evaporation at the soil surface, and (d) transpiration by plants. The UNSAT-H code was verified and benchmarked by Baca and Magnuson (1990) and was successfully applied to simulate moisture transport at several semi-arid locations (Fayer et al, 1992;Baca et al, 1992;Magnuson, 1993;Martian and Magnuson, 1993).…”
Section: Selected Modelmentioning
confidence: 99%