农业环境科学学报
農業環境科學學報
농업배경과학학보
Journal of Agro-Environment Science
2014年
7期
1358-1365
,共8页
吕雪艳%姚遥%孙媛媛%吴吉春%郭红岩
呂雪豔%姚遙%孫媛媛%吳吉春%郭紅巖
려설염%요요%손원원%오길춘%곽홍암
土壤胶体%释放%离子强度%pH%扰动土柱%原状土柱
土壤膠體%釋放%離子彊度%pH%擾動土柱%原狀土柱
토양효체%석방%리자강도%pH%우동토주%원상토주
soil colloid%release%ionic strength%pH%disturbed column%undisturbed column
采用实验室土柱纵向淋溶法,研究了离子强度及pH变化对常熟乌栅土原状、扰动土柱以及东北黑土、江西红壤扰动土柱土壤胶体释放的影响。结果表明离子强度变化对我国不同类型土壤胶体释放影响不同:淋洗液电解质为NaCl时,对于常熟乌栅土以及东北黑土,离子强度减小促进胶体的释放,反之抑制胶体的释放;对于江西红壤,离子强度变化对土壤胶体释放则不产生影响。淋洗液电解质为CaCl2条件下,土壤胶体的释放量低于淋洗液为NaCl,且离子强度变化对三种土壤胶体的释放均不产生明显影响。相同条件下,常熟乌栅土及东北黑土胶体释放量远远大于江西红壤,pH变化则对上述类型土壤胶体释放的影响不明显。研究结果有助于进一步阐明水化学条件的变化对我国不同类型土壤胶体释放的影响规律。
採用實驗室土柱縱嚮淋溶法,研究瞭離子彊度及pH變化對常熟烏柵土原狀、擾動土柱以及東北黑土、江西紅壤擾動土柱土壤膠體釋放的影響。結果錶明離子彊度變化對我國不同類型土壤膠體釋放影響不同:淋洗液電解質為NaCl時,對于常熟烏柵土以及東北黑土,離子彊度減小促進膠體的釋放,反之抑製膠體的釋放;對于江西紅壤,離子彊度變化對土壤膠體釋放則不產生影響。淋洗液電解質為CaCl2條件下,土壤膠體的釋放量低于淋洗液為NaCl,且離子彊度變化對三種土壤膠體的釋放均不產生明顯影響。相同條件下,常熟烏柵土及東北黑土膠體釋放量遠遠大于江西紅壤,pH變化則對上述類型土壤膠體釋放的影響不明顯。研究結果有助于進一步闡明水化學條件的變化對我國不同類型土壤膠體釋放的影響規律。
채용실험실토주종향림용법,연구료리자강도급pH변화대상숙오책토원상、우동토주이급동북흑토、강서홍양우동토주토양효체석방적영향。결과표명리자강도변화대아국불동류형토양효체석방영향불동:림세액전해질위NaCl시,대우상숙오책토이급동북흑토,리자강도감소촉진효체적석방,반지억제효체적석방;대우강서홍양,리자강도변화대토양효체석방칙불산생영향。림세액전해질위CaCl2조건하,토양효체적석방량저우림세액위NaCl,차리자강도변화대삼충토양효체적석방균불산생명현영향。상동조건하,상숙오책토급동북흑토효체석방량원원대우강서홍양,pH변화칙대상술류형토양효체석방적영향불명현。연구결과유조우진일보천명수화학조건적변화대아국불동류형토양효체석방적영향규률。
Colloid mobilization would facilitate pollutant transport in the environment. In laboratory, leaching experiments were performed to investigate the effects of ionic strength and pH on colloid release from undisturbed and disturbed Wushan soil columns from Changshu, dis-turbed black soil column from northeast China(Dongbei)and disturbed red soil column from Jiangxi. The effects of ionic strength on colloid release were significantly different in various soils. In the electrolyte NaCl system, increasing ionic strength obviously reduced the release capacity of soil colloids for Changshu Wushan soil and Dongbei black soil, while ionic strength had little effects on collois release in Jiangxi red soil. In electrolyte CaCl2 system, however, ionic strength had no significant impacts on soil collois release. Moreover, colloid release was much smaller in CaCl2 than in NaCl. Under the same conditions of solution chemistry, the amount of colloid released was far greater in Changshu Wushan soil and Dongbei black soil than in Jiangxi red soil. pH showed little influence on colloid release. The research findings would be useful for further understanding the impacts of water chemical conditions on colloid release of different soils.