Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.2136/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
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ISSN | 0361-5995 |
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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