Methodological approach for evaluating the response of soil hydrological behavior to irrigation with treated municipal wastewater

被引:66
|
作者
Coppola, A
Santini, A
Botti, P
Vacca, S
Comegna, V
Severino, G
机构
[1] Univ Basilicata, Dipartimento DITEC, I-85100 Potenza, Italy
[2] Univ Naples Federico II, Dipartimento Ingn Agraria & Agron, Portici, Italy
[3] Settore Salvaguardia Territorio & Corpi Idrici En, Cagliari, Italy
[4] Univ Sassari, Dipartimento Bot & Ecol Vegetale, Sassari, Italy
关键词
wastewater reuse; soil water flow and solute transport; transport mechanism;
D O I
10.1016/j.jhydrol.2003.12.028
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
This paper aims mainly to provide experimental evidence of the consequences of urban wastewater reuse in irrigation practices on the hydrological behavior of soils. The effects on both the hydraulic and dispersive properties of representative soils in southern Sardinia are illustrated. Ten undisturbed soil monoliths. 120 cm in height and 40 cm in diameter, were collected from plots previously selected through a soil survey. Soil hydraulic and solute transport properties were determined before and after application of wastewater using transient water infiltration and steady state-solute transport column experiments. Detailed spatial -temporal information on the propagation of water and solute through the soil profiles were obtained by monitoring soil water contents, theta. pressure heads, h, and solute concentrations, C, measured by a network of time domain reflectometry probes, tensiometers and solution samplers horizontally inserted in each column at different depths. A disturbed layer at the soil surface, which expands in depth with time, was observed, characterized by reduced soil porosity, translation of pore size distribution towards narrower pores and consequent decrease in water retention, hydraulic conductivity and hydrodynamic dispersion. It is shown that these changes occurring in the disturbed soil layer, although local by nature, affect the hydrological behavior of the whole soil profile. Due to the disturbed layer formation, the soil beneath never saturates. Such behavior has important consequences on the solute transport in soils, as unsaturated conditions mean hi,,her residence times of solutes, even of those normally characterized by considerable mobility (e.g. boron), which may accumulate along the profile. The results mainly provide experimental evidence that knowledge of the chemical and microbiological composition of the water is not sufficient to evaluate its suitability for irrigation. Other factors, mainly soil physical and hydrological characteristics, should be considered in order to define appropriate guidelines for wastewater management. (C) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:114 / 134
页数:21
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