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Programa de agua y saneamiento para la zona rural de la cuenca baja del rio Nigua. Trabajo de grado para la obtencion del grado de Ingeniero Civil
1993
Demorizi Lerebours, H. R.Jerez Almonte, M. L.Ortiz Olivo, C.
Simplification of the Gardner model: effects on maximum upward flux in the presence of a shallow water table | Simplification du modèle de Gardner: effets sur le flux ascendant en présence d’une nappe phréatique peu profonde Simplificación del modelo de Gardner: efectos sobre el flujo ascendente máximo en presencia de un nivel freático superficial Gardner模型简化对地下水浅埋条件极限蒸发强度的影响 Simplificação do modelo de Gardner: efeitos do fluxo vertical máximo pela presença de níveis de água rasos 全文
2018
Xing, Xuguang | Ma, Xiaoyi
The maximum upward flux (Eₘₐₓ) is a control condition for the development of groundwater evaporation models, which can be predicted through the Gardner model. A high-precision Eₘₐₓ prediction helps to improve irrigation practice. When using the Gardner model, it has widely been accepted to ignore parameter b (a soil-water constant) for model simplification. However, this may affect the prediction accuracy; therefore, how parameter b affects Eₘₐₓ requires detailed investigation. An indoor one-dimensional soil-column evaporation experiment was conducted to observe Eₘₐₓ in the presence of a water table of depth 50 cm. The study consisted of 13 treatments based on four solutes and three concentrations in groundwater: KCl, NaCl, CaCl₂, and MgCl₂, with concentrations of 5, 30, and 100 g/L (salty groundwater); distilled water was used as a control treatment. Results indicated that for the experimental homogeneous loam, the average Eₘₐₓ for the treatments supplied by salty groundwater was larger than that supplied by distilled water. Furthermore, during the prediction of the Gardner-model-based Eₘₐₓ, ignoring b and including b always led to an overestimate and underestimate, respectively, compared to the observed Eₘₐₓ. However, the maximum upward flux calculated including b (i.e. Ebₘₐₓ) had higher accuracy than that ignoring b for Eₘₐₓ prediction. Moreover, the impact of ignoring b on Eₘₐₓ gradually weakened with increasing b value. This research helps to reveal the groundwater evaporation mechanism.
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