Arid
DOI10.2136/sssaj1999.03615995006300030018x
Wastewater effects on montmorillonite suspensions and hydraulic properties of sandy soils
Tarchitzky, J; Golobati, Y; Keren, R; Chen, Y
通讯作者Chen, Y
来源期刊SOIL SCIENCE SOCIETY OF AMERICA JOURNAL
ISSN0361-5995
出版年1999
卷号63期号:3页码:554-560
英文摘要

Recycled wastewater eluent is an important source of irrigation water in arid and semiarid regions. In these regions, however, irrigation water quality is one of the main factors limiting plant growth Wastewater effluents generally contain high concentrations of suspended and dissolved solids, both organic and inorganic. Inorganic dissolved solids me only minimally removed from the effluent during conventional sewage treatment (secondary or tertiary). As a result, most of the salts added during domestic and industrial usage remain in the irrigation wafer and may eventually reach the soil, A number of researchers have reported reduced hydraulic conductivity for soils to which treated wastewater has been applied. In this research, the influence of dissolved organic matter (DOM) contained in reclaimed wastewater effluents (mainly humic substances) on the flocculation of montmorillonite and on the hydraulic properties of sobs was studied. Flocculation values (FVs) for Na-montmorillonite increased with increasing concentrations of DOM at all pH levels analyzed (5.5, 7.0, and 8.5), Maximum FV levels were exhibited for Na-montmorillonite at the highest DONI concentrations. The effect of DOM on FV can be explained by the mechanisms of edge-charge reversal and mutual flocculation. The hydraulic conductivity (HC) of a sandy soil was determined in the laboratory by leaching columns with an electrolyte solution chemically similar to that of the wastewater effluent (but without DOM). In columns treated with wastewater effluent, the HC exhibited a-sharp decrease to only 20% of its initial value. The adverse effect of DOM on HC was evident for this soil despite a relatively low exchangeable sodium percentage (ESP). The reduction in KC is likely to be the result of decreased soil pore-size, which reflects two processes: (i) retention of part of the DOM during water percolation; and (ii) a change in pore-size distribution due to swelling and dispersion of clay particles. The latter may result from a higher percentage of adsorbed sodium combined with the presence of humic substances from the wastewater effluent.


类型Article
语种英语
国家Israel
收录类别SCI-E
WOS记录号WOS:000081490700018
WOS关键词HUMIC SUBSTANCES ; IRON-OXIDES ; FLOCCULATION ; DISPERSION ; CONDUCTIVITY ; COAGULATION ; PARTICLES ; CLAYS
WOS类目Soil Science
WOS研究方向Agriculture
来源机构Hebrew University of Jerusalem
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/138231
作者单位(1)Hebrew Univ Jerusalem, Fac Agr Food & Environm Qual Sci, Dept Soil & Water Sci, IL-76100 Rehovot, Israel;(2)Minist Agr, Field Serv, Extens Serv, IL-61070 Tel Aviv, Israel;(3)Agr Res Org, Volcani Ctr, Inst Soils & Water, IL-50250 Bet Dagan, Israel
推荐引用方式
GB/T 7714
Tarchitzky, J,Golobati, Y,Keren, R,et al. Wastewater effects on montmorillonite suspensions and hydraulic properties of sandy soils[J]. Hebrew University of Jerusalem,1999,63(3):554-560.
APA Tarchitzky, J,Golobati, Y,Keren, R,&Chen, Y.(1999).Wastewater effects on montmorillonite suspensions and hydraulic properties of sandy soils.SOIL SCIENCE SOCIETY OF AMERICA JOURNAL,63(3),554-560.
MLA Tarchitzky, J,et al."Wastewater effects on montmorillonite suspensions and hydraulic properties of sandy soils".SOIL SCIENCE SOCIETY OF AMERICA JOURNAL 63.3(1999):554-560.
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