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王勤静 《石油化工环境保护》1996,(3):1-5
应用非水电位滴定法测定了废水中各种烷基磷酸酯钾盐及其单、双酯盐。方法的变异系数分别为2.3%和7.8%(n=12)。本法可有效地消除非离子表面活性剂的干扰,适用于化纤油剂的质量检验和上油槽中油剂浓度的测定。 相似文献
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ThebufferingeffectsofaquaticsedimentsagainstacidicdepositionLiaoBohan;TangHongxiao(ResearehCenterforEco-EnvironmentalSciences... 相似文献
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1IntroductionCalciumchlorideisoftenusedinthefieldofsoilstabilizationandraisingdustcontrolbecauseitcanreactwithwaterglas(Wu,19... 相似文献
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IntroductionSurfactantsenhancetheremediationofNAPL contaminatedsitesbyincreasingtheaqueous phaseconcentrationoftheNAPLviamicelleformation ,microemulsification ,ormobilizingtheNAPLphase (Kile ,1989;Edwards,1991;Guha ,1998a ;Ko ,1998;Zimmerman ,1999;Bettahar,1999;Willson ,1999;Pa… 相似文献
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Yilei Yu Xianfang Song Yinghua Zhang Fandong Zheng Ji Liang Dongmei Han Ying M Hongmei Bu 《环境科学学报(英文版)》2013,25(9):1754-1763
Reclaimed water was successfully used to recover the dry Chaobai River in Northern China, but groundwater may be polluted. To ensure groundwater protection, it is therefore critical to identify the governing factors of groundwater chemistry. Samples of reclaimed water, river and groundwater were collected monthly at Chaobai River from January to September in 2010. Fifteen water parameters were analyzed. Two kinds of reclaimed water were different in type (Na-Ca-Mg-Cl-HCO3 or Na-Ca-Cl-HCO3 ) and concentration of nitrogen. The ionic concentration and type in river were similar to reclaimed water. Some shallow wells near the river bed had the same type (Na-Ca-Mg-Cl-HCO3 ) and high concentration as reclaimed water, but others were consistent with the deep wells (Ca-Mg-HCO3 ). Using cluster analysis, the 9 months were divided into two periods (dry and wet seasons), and all samples were grouped into several spatial clusters, indicating different controlling mechanisms. Principal component analysis and conventional ionic plots showed that calcium, magnesium and bicarbonate were controlled by water-rock interaction in all deep and some shallow wells. This included the dissolution of calcite and carbonate weathering. Sodium, potassium, chloride and sulfate in river and some shallow wells recharged by river were governed by evaporation crystallization and mixing of reclaimed water. But groundwater chemistry was not controlled by precipitation. During the infiltration of reclaimed water, cation exchange took place between (sodium, potassium) and (calcium, magnesium). Nitrification and denitrification both happened in most shallow groundwater, but only denitrification in deep groundwater. 相似文献
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采用离子色谱法同时测定白云石中高含量钙镁,该法与目前使用的络合滴定法相比,具有准确可靠、操作简便快速、无干扰等特点。对样品测定取得了满意的结果,氧化钙与镁瓣含量分别为31.99%和21.47%,相对标准偏差分别为0.81%和0.65%,平均回收率分别99.9%和102%。 相似文献