阳极溶出伏安法快速测定地表水中镉

利用阳极溶出伏安法原理,采用PDV 6000型重金属快速分析仪测定地表水中的镉。在1.25μg/L~40.0μg/L范围内,质量浓度与阳极溶出峰电流和峰面积呈良好的线性关系,方法检出限为0.001 mg/L,水样平行测定的RSD为8.9%,加标回收率为80.5%~118%,与石墨炉原子吸收光谱法的测定结果基本一致。     

气相色谱法测定地表水中百菌清和菊酯类农药

采用正己烷萃取地表水中的百菌清和6种菊酯类农药,通过毛细管气相色谱法-电子捕获检测器(GC-ECD)定性定量。供试农药的线性范围:百菌清为10.0μg/L～200μg/L,6种菊酯类为50.0μg/L～1 000μg/L;方法检出限分别为:百菌清0.054μg/L,甲氰菊酯0.62μg/L,三氟氯氰菊酯0.68μg/L,氯菊酯0.40μg/L,氯氰菊酯0.65μg/L,氰戊菊酯0.78μg/L,溴氰菊酯0.15μg/L;对地表水样品3个质量浓度水平的平均加标回收率为91.3%～118%,6次平行测定的RSD<5%。     

超高压液相色谱/质谱联用法测定地表水中特定污染物

采用超高压液相色谱/质谱联用法测定地表水特定项目中包括微囊藻毒素-LR在内的13种污染物,对测定条件进行优化,使得各目标化合物均能在3min内检测完毕.试验表明,方法在各测定范围内线性良好,相关系数均〉0.99,各目标化合物的方法检出限为0.12μg/L～8.40μg/L,地表水样的加标回收率在62.0% ～104%之间,6次平行测定的RSD〈6%.用该方法测实际水样,阿特拉津和马拉硫磷被检出,质量浓度分别为0.6μg/L和0.7μg/L.     

国家地表水水质自动监测网的建设与运行

总结了中国地表水水质自动监测网的建设运行与应用现状,分析了水站目前在运行管理、数据质量保证和质量控制中存在的问题,并就今后利用水质自动监测数据进行综合分析以及保障水质自动监测的可持续发展提出了意见和建议。     

紫外分光光度法测定水和废水中硫化物

对紫外分光光度法测定水和废话中硫化物的方法进行了研究,试验了稳定时间、干扰物质、碱溶液浓度对测定的影响,提出了最佳测定条件。该方法检测限为０．０４ｍｇ／Ｌ,相对标准偏为１．４％,加标回收率在９１．６％～１０１．９％之间。     

Spatio-temporal variations in water quality of Nullah Aik-tributary of the river Chenab, Pakistan

This study reports the spatio-temporal changes in water quality of Nullah Aik, tributary of the Chenab River, Pakistan. Stream water samples were collected at seven sampling sites on seasonal basis from September 2004 to April 2006 and were analyzed for 24 water quality parameters. Most significant parameters which contributed in spatio-temporal variations were assessed by statistical techniques such as Hierarchical Agglomerative Cluster Analysis (HACA), Factor Analysis/Principal Components Analysis (FA/PCA), and Discriminant Function Analysis (DFA). HACA identified three different classes of sites: Relatively Unimpaired, Impaired and Less Impaired Regions on the basis of similarity among different physicochemical characteristics and pollutant level between the sampling sites. DFA produced the best results for identification of main variables for temporal and spatial analysis and separated eight parameters (DO, hardness, sulphides, K, Fe, Pb, Cr and Zn) that accounted 89.7% of total variations of spatial analysis. Temporal analysis using DFA separated six parameters (E.C., TDS, salinity, hardness, chlorides and Pb) that showed more than 84.6% of total temporal variation. FA/PCA identified six significant factors (sources) which were responsible for major variations in water quality dataset of Nullah Aik. The results signify that parameters identified by statistical analyses were responsible for water quality change and suggest the possibility of industrial, municipal and agricultural runoff, parent rock material contamination. The results suggest dire need for proper management measures to restore the water quality of this tributary for a healthy and promising aquatic ecosystem and also highlights its importance for objective ecological policy and decision making process.     

UPLC-MS/MS法同时测定地表水中多种有机污染物

采用超高效液相色谱-串联质谱法直接进样测定地表水中26种有机污染物,通过优化试验条件,使各目标化合物在1.00μg/L^100μg/L范围内线性良好,相关系数(r 2)>0.995,方法检出限为0.003μg/L^1.0μg/L。将该方法用于地表水样的测定,加标回收率为79.0%~120%,6次测定结果的RSD均<15%。     

地表水环境质量评价办法在应用中存在的问题及建议

分析了《地表水环境质量评价办法(试行)》在应用过程中显现的问题,提出了增加地区特征污染物污染情况说明,补充水质状况定性评价特殊情况说明和变化趋势评价方法的判断优先级别,明确数据修约方式、检出限以下测值的评价方法及水质类别不同而标准限值相同的指标评价方法等建议。     

水中草甘膦和氨甲基膦酸的柱前衍生-液相色谱方法研究

建立柱前衍生-液相色谱-荧光检测法同时测定水中草甘膦和氨甲基膦酸的方法。水样经芴甲氧羰酰氯衍生化后取上清液进样,采用ODS C18柱,以水(5 mmol/L乙酸铵)-乙腈作为流动相进行梯度洗脱,采用荧光检测器进行检测。实验通过加入柠檬酸三钠,解决了实际水样中金属阳离子的干扰问题。草甘膦和氨甲基膦酸在一定范围内线性良好(r=0.997 3~0.999 0),回收率为92.2%~102%,相对标准偏差为4.3%~8.5%,方法检出限为1.29μg/L和1.84μg/L。     

Model Development for Nutrient Loading Estimates from Paddy Rice Fields in Korea

Abstract

A field experiment was performed to evaluate water and nutrient balances in paddy rice culture operations during 2001–2002. The water balance analysis indicated that about half (50–60%) of the total outflow was lost by surface drainage, with the remainder occurring by evapotranspiration (490–530 mm). The surface drainage from paddy fields was mainly caused by rainfall and forced-drainage, and in particular, the runoff during early rice culture periods depends more on the forced-drainage due to fertilization practices. Most of the total phosphorus (T-P) inflow was supplied by fertilization at transplanting, while the total nitrogen (T-N) inflow was supplied by the three fertilizations, precipitation, and from the upper paddy field, which comprised 13–33% of the total inflow. Although most of the nutrient outflow was attributed to plant uptake, nutrient loss by surface drainage was substantial, comprising 20% for T-N and 10% for T-P. Water and nutrient balances indicate that reduction of surface drainage from paddy rice fields is imperative for nonpoint source pollution control. The simplified computer model, PADDIMOD, was developed to simulate water and nutrient (T-N and T-P) behavior in the paddy rice field. The model predicts daily ponded water depth, surface drainage, and nutrient concentrations. It was formulated with a few equations and simplified assumptions, but its application and a model fitness test indicated that the simulation results reasonably matched the observed data. It is a simple and convenient planning model that could be used to evaluate BMPs of paddy rice fields alone or in combination with other complex watershed models. Application of the PADDIMOD to other paddy rice fields with different agricultural environments might require further calibration and validation.