Point- and nonpoint-source pesticide contamination in the Zwester Ohm catchment, Germany

Reducing pesticide loads in surface waters implies identifying the pathways responsible for the pollution. The current study documents the pesticide contamination of the river Zwester Ohm, a 4917-ha catchment in Germany with 41% of the land used for crop production. Discharges and concentrations of 19 pesticides were measured continuously at three locations for 15 mo. The load detected at the outlet of the catchment amounted to 9048 g a.i. The losses represent 0.22% of the pesticides applied by the farmers. The contamination showed a seasonal pattern following the pesticide application times. The wastewater treatment plant system (WWTPS) in the catchment (two wastewater treatment plants [WWTP], 14 combined sewer overflows (CSO), four CSO tanks) emits during dry weather periods purified sewage and during storm events sewage mixed with stormwater runoff into the river. The contribution by the WWTPS to the pesticide load was defined as point-source pollution (PSP). The load was dominated by PSP with at least 77% of the total pollution. No significant interdependencies between intrinsic properties of the pesticides, hydrometeorological factors, and the loads occurring in the stream could be found. Therefore, it is not possible to predict PSP for other catchments based on the results from this study. Whereas 65% of the total load entered the river via the WWTP, a portion of 12% was attributed to the CSO. The study points out that the influence of CSO on PSP should be taken into account in future catchment studies in areas with comparable agricultural structure.     

Acrylamid in Lebensmitteln

Ohne Zusammenfassung     

锡林河流域地表水水化学主离子特征及控制因素

通过对2006~2008年锡林河主要径流期内13个河水断面239个水样以及同期地下水和大气降水主离子水化学进行分析,结合锡林河流域的气象和水文资料,利用Piper三线图和Gibbs图分析了锡林河河水的水化学特征及主离子组成变化特征.结果表明,锡林河河水TDS变化范围在136.7~376.5 mg·L-1之间,平均245.1 mg·L-1,为低矿化度河水;河水中主要阳离子以Ca2+为主,阴离子以HCO-3为主,河水的水化学类型从HCO-3-Ca2+过渡到HCO-3-Ca2+·Mg2+;河水主离子平均浓度年内、年际变化均不大,年内变化表现在5月主离子浓度高于其他月,年际变化表现为主离子在2007年的平均浓度均较小;空间上,Ca2+、Na+、Mg2+、K+、Cl-和HCO-3的浓度呈现沿程逐渐增加的趋势,SO2-4的浓度变化呈先增加后减小的趋势;河水中主离子浓度值介于大气降水和地下水之间,并且十分接近地下水浓度,说明地表水同时受大气降水和地下水补给并主要依靠地下水补给;Gibbs图显示河水离子组成主要与流域内的岩石风化有关,流域有一定量的蒸发岩存在,但蒸发岩对水化学的贡献弱于碳酸盐岩.