东营市地下水碘化物的空间分布特征及影响分析

为研究东营市地下水碘化物的空间分布特征以及对环境和饮用水安全的影响,对域内的山前平原区和黄泛平原区分别布设了48个和47个调查点位。结果表明:东营市地下水碘化物质量浓度均值达到(0.247±0.263) mg/L,其环境质量呈现由南向北逐步恶化的变化趋势,超过90%的国土面积处于地下水环境质量标准Ⅳ类。山前平原区南部是东营市唯一具备可饮用地下水的区域,域内以适碘地区为主,缺碘地区和高碘地区分别位于区域东南部和第二次海侵古海岸线附近。总体上,可饮用地下水处于中等缺碘水平,海(咸)水入侵已成为影响可饮用地下水适碘地区范围的关键因素,需引起高度关注。地下水所处的环境地质概况、海(咸)水入侵和大气降水是影响碘化物空间分布的重要因素。     

新疆平原区饮用地下水中F-含量的调查与评价

利用1997—1999年2058个饮用地下水中F-含量的测试成果。评价了新疆平原区饮用地下水中F-含量的状况,其结果为：F-含量变化范围为0．05—7．00mg/L,面积加权平均值为0．68mg/L,超标率18．9％。     

遂宁城乡集中式饮用水水源地钡分布特征及健康风险评价

为考察遂宁市辖区内集中式饮用水水源地污染物钡的分布特征和健康风险水平,通过电感耦合等离子体原子发射光谱法对研究区域内市级、县级和乡镇级所有在用的56个集中式饮用水水源地钡的浓度进行分析检测,借助空间分析与统计分析的结果,探讨了其空间分布和浓度差异,并利用环境健康风险评价模型,对不同类型水源地钡的健康风险进行了评价。结果表明,38个地表水水源地钡的浓度范围为0.065~0.180 mg/L,均值为0.110 mg/L;18个地下水水源地钡的浓度范围为0.027~0.370 mg/L,均值为0.130 mg/L。地表水与地下水水源地间钡的浓度差异具有统计学意义(P0.05),钡的空间分布也存在不同程度的差异性。各水源地中的钡经饮用和皮肤暴露两种途径对成人和儿童所引起的非致癌风险值为1.34×10~(-8)~1.62×10~(-8),远低于推荐的最大可接受风险水平(1.0×10~(-6)),各水源地因污染物钡导致的非致癌风险极低。     

南通平原河网地区典型农田系统地下水硝态氮污染调查

针对平原河网地区典型农田系统灌溉施肥带来的地下水环境污染问题,采集南通地区蔬菜地、水稻-小麦轮作地、水稻-油菜轮作地和桑地地下水样品,分析了不同农田种植体系下的地下水污染程度。结果表明,蔬菜、桑地、水稻-油菜轮作、水稻-小麦轮作地地下水的硝态氮(N)平均值分别为12.2,9.53,7.95和6.12 mg/L,与氮肥用量呈显著的正相关关系;研究区域地下水硝态氮超Ⅲ类标准率(20 mg/L)的为4.8%,表明地下水已部分受到硝态氮污染。     

万峰湖总有机碳空间分布特征

于2012年9月对万峰湖(水库)的总有机碳(TOC)空间分布特征进行研究,结果显示:TOC含量范围为0.41~3.94 mg/L。TOC在纵向分布上的差异不显著,在垂向分布上,总体呈现出上层中层下层的趋势。TOC在垂向上的分布差异主要源于万峰湖属于深水水库,不同深度水层因光照和温度差异所导致生物量的多寡是致使万峰湖出现上层TOC浓度明显高于中层和下层的主要因素。     

桂林市相思江流域氮磷分布特征解析及空间变化预测

通过2019年6—12月对相思江流域（临桂段）丰水期和枯水期的水质监测分析,并采用主成分分析（PCA）对污染初步溯源和反距离加权插值（IDW）对氮磷质量浓度空间变化插值预测。结果表明：研究区内氮磷污染严重,TN和TP质量浓度范围分别为0.312 mg/L～14.744 mg/L和0.004 mg/L～0.452 mg/L,TN质量浓度枯水期高于丰水期,TP两水期大致相等。研究区内非点源氮磷呈现出明显空间变异性,上游氮磷污染最为严重。农业面源污染中禽畜养殖和生活污水是流域内主要污染因子。     

重庆典型岩溶地区地下水多环芳烃污染水平及健康风险

采集重庆3个典型岩溶地区113个地下水样品,利用人体暴露风险系数法对16种优先控制多环芳烃(PAHs)饮水途径健康风险进行评价。结果表明:地下水中PAHs、致癌PAH和BaP的质量浓度分别为200 ng/L～2 638 ng/L、未检出～362 ng/L和未检出～62.7 ng/L,其中南川区地下水中BaP质量浓度为45.1 ng/L,已超过《生活饮用水卫生标准》(GB 5749—2006)的水质要求。PAHs污染水平为南川区老龙洞流域青木关流域,与国内其他岩溶地区地下水相比,处于较高污染水平。人群的致癌风险(ILCR)为5×10~(-10)～2.80×10~(-5),其中南川区ILCR10~(-6),具有潜在致癌风险;非致癌类PAHs饮水途径健康风险处于10~(-11)～10~(-9)水平,远低于USEPA规定的阈值1。     

三峡库区重庆段淹没区土壤重金属分布及评价

三峡库区重庆段淹没区土壤重金属含量均低于国家土壤环境标准三级,其中铜含量范围为10.7~80.2mg/kg,均值为37.0 mg/kg;铅含量范围为14.6~51.8mg/kg,均值为29.3mg/kg;锌含量范围为47.5~93.3mg/kg,均值为72.7mg/kg;镉含量范围为0.084~0.765mg/kg,均值为0.321mg/kg;汞含量范围为0.032~0.204mg/kg,均值为0.059mg/kg;砷含量范围为4.63~12.7mg/kg,均值为8.65mg/kg。三峡库区淹没区土壤主要受镉铜污染和铅镉污染。     

丹江口水库流域氮素时空分布特征

为全面了解丹江口水库流域氮素污染状况,对库区26个点位及10条主要入库河流入库口处的表层水样进行了丰水期、平水期、枯水期采样与监测,探讨了氮素时空分布特征。入库口总氮检出范围为1.31~10.96 mg/L,其中泗河和神定河入库口总氮最高。总氮为库区水质主要限制因子,年均总氮质量浓度为1.13~2.71 mg/L;汉江库区整体上总氮污染水平略高于丹江库区,且与丹江库区相比,汉江库区受点源排放的影响较大。10条入库河流总氮的总年均输入量为63 347.31 t/a,其中汉江的总氮输入量最大;入库河流总氮控制的关键在于溶解性有机氮和硝酸盐氮的控制。     

BOD快速测定仪的日常使用与维护

样品浓度影响到微生物膜上菌种的活性。在仪器的适用范围内,菌种活性的变化可分为四个阶段,即2~5mg/L、5~13mg/L、13~30mg/L、30~50mg/L。为了获得样品的准确浓度,需在这四个浓度范围内分别取两点进行点控,样品的精密度变差可以作为更换管路的一个依据。灵敏度下降表明,应该更换微生物膜。     

Assessment of groundwater pollution in West Delhi, India using geostatistical approach

The exploration, exploitation, and unscientific management of groundwater resources in the National Capital Territory (NCT) of Delhi, India have posed a serious threat of reduction in quantity and deterioration of quality. The objective of the study is to determine the groundwater quality and to assess the risk of groundwater pollution at Najafgarh, NCT of Delhi. The groundwater quality parameters were analyzed from the existing wells of the Najafgarh and the thematic maps were generated using geostatistical concepts. Ordinary kriging and indicator kriging methods were used as geostatistical approach for preparation of thematic maps of the groundwater quality parameters such as bicarbonate, calcium, chloride, electrical conductivity (EC), magnesium, nitrate, sodium, and sulphate with concentrations equal or greater than their respective groundwater pollution cutoff value. Experimental semivariogram values were fitted well in spherical model for the water quality parameters, such as bicarbonate, chloride, EC, magnesium, sodium, and sulphate and in exponential model for calcium and nitrate. The thematic maps of all the groundwater quality parameters exhibited an increasing trend of pollution from the northern and western part of the study area towards the southern and eastern part. The concentration was highest at the southernmost part of the study area but it could not reflect correctly the groundwater pollution status. The indicator kriging method is useful to assess the risk of groundwater pollution by giving the conditional probability of concentrations of different chemical parameters exceeding their cutoff values. Thus, risk assessment of groundwater pollution is useful for proper management of groundwater resources and minimizing the pollution threat.     

淮河流域江苏平原区浅层地下水污染分析

以淮河流域江苏平原区浅层地下水为研究对象，通过对当地影响较大的污染源调查采样，分析了该地区所采602组水样的无机和有机污染状况。研究表明，区内浅层地下水无机污染较严重，基本形成面状污染，地下水超标率高达83．4％，超标率最高为碘化物。有机污染物检出率34．2％，主要包括二氯甲烷、萘和1，2-二氯乙烷等，以点状分布为主。在此基础上阐述了大气降水、污水灌溉、农业施肥以及地下水开采等人类活动对浅层地下水的影响和污染状况。     

再生铅企业土壤-地下水中重金属污染迁移特征

为了解某再生铅企业厂区土壤和浅层地下水重金属污染状况,采集了96个土壤样品和4个地下水样品,定量分析了其Pb,Cd,As的含量及空间分布特征,探讨企业生产对环境造成的影响。结果表明,该区域土壤中Cd、As、Pb超标率分别为67.0%,35.1%,11.7%,在厂区呈现局部富集现象,最大值是土壤背景值的几十倍乃至数千倍;在垂直方向上由于Pb,Cd,As在土壤中迁移率较低,其值随深度增加呈总体下降趋势;该区域地下水中Pb,Cd,As值远低于地下水质量标准值。     

长沙市某集中式饮用水水源地周边土壤重金属污染特征和风险评价

以长沙某河库兼用型饮用水水源地一、二级保护区土壤为研究对象,于2018年8月采用网格布点法在一级和二级保护区分别布设3个和7个采样点,在水源地历史采样区布设5个采样点,探究土壤中Cd、Pb、Cr、Cu、Zn、Ni、Hg、As的含量分布及污染水平。结果表明：土壤中As、Cd、Cr、Cu、Hg、Ni、Pb、Zn的含量均值分别为46.56、4.90、81.87、46.64、0.19、30.11、75.11、237.93 mg/kg。重金属元素含量均值超过农用地污染风险筛选值的样品占比排序为Cd （86.7%）>Zn （60%）>As （53.3%）>Cu （6.7%）=Pb （6.7%）。土壤中As、Cd、Cr、Cu、Hg、Ni、Pb、Zn的单因子污染指数分别为1.55、16.34、0.41、0.47、0.08、0.30、0.63、0.95,主要为Cd、As污染。研究区土壤重金属综合污染指数为11.71,属重污染等级。水源地一级保护区、二级保护区、历史采样区2018年、历史采样区2014年土壤重金属综合污染指数分别为20.41、14.94、1.98、1.17。后期应加强对该饮用水水源地土壤中Cd、Pb、Cu、Zn、As的污染控制和治理。     

Analysis of spatial–temporal distributions of nitrate-N concentration in Shitoukoumen catchment in northeast China

This article discusses the generation and migration process of nitrate-N pollution in shallow groundwater caused by agricultural nonpoint source pollution in the catchment area of Shitoukoumen Reservoir in northeast China. By monitoring the shallow groundwater nitrate-N in the low-water period, the normal season, and high-flow period in the study area for a year, it was found that the nitrate-N concentration in the shallow groundwater of this area had a seasonal variation in both spatial and time distribution. In the time distribution, the peak value appeared in July, the high-flow period, and the valley value appeared in April, the low-water period, and showed a significant correlation with the time distribution of fertilization rate and rainfall. In the spatial distribution of nitrate-N pollution, when the distribution in shallow groundwater was analyzed separately in the three different periods (low-water period, the normal season, and high-flow period) and the discipline transference and enrichment of nitrate-N pollution in shallow groundwater was determined, this indicated that the region in the southeast study area where runoff conditions were better was less contaminated, and the region where runoff conditions were poor, as well as the region along the river were seriously polluted. The nitrate-N concentration in shallow groundwater was distributed mainly along the path of groundwater flow and was excreted in the drainage region. This showed that the spatial distribution of nitrate-N concentration in the shallow groundwater of the entire region was mainly controlled by the groundwater flow system. At the same time, in the middle and lower reaches of the study area, the seasonal changes in the recharged–excreted relationship between groundwater and river caused seasonal differences in the spatial distribution of nitrate-N pollution in groundwater. The combined effects of the groundwater mobility and the surface river resulted in a poor correlation between the groundwater nitrate-N concentration and land-use types. Only in the plain area where there was little influence from groundwater runoff and the surface river did the groundwater nitrate-N concentration correlate with land-use types. The spatial and time distribution of nitrate-N concentration in the shallow groundwater of the study area was impacted by agricultural nonpoint source pollution, the groundwater flow system, and the surface river and formed a concentration response system which uses basins as a unit.     

Fluoride, boron and nitrate toxicity in ground water of northwest Rajasthan, India

The study was carried out to access the fluoride, boron, and nitrate concentrations in ground water samples of different villages in Indira Gandhi, Bhakra, and Gang canal catchment area of northwest Rajasthan, India. Rural population, in the study site, is using groundwater for drinking and irrigation purposes, without any quality test of water. All water samples (including canal water) were contaminated with fluoride. Fluoride, boron, and nitrate were observed in the ranges of 0.50–8.50, 0.0–7.73, and 0.0–278.68 mg/l, respectively. Most of the water samples were in the categories of fluoride 1.50 mg/l, of boron 2.0–4.0 mg/l, and of nitrate <?45 mg/l. There was no industrial pollution in the study site; hence, availability of these compounds in groundwater was due to natural reasons and by the use of chemical fertilizers.     

镇江地区土壤样品中重金属Cd含量与空间分布

通过对镇江地区土壤样品中 Cd 监测结果统计分析表明，全市69个样品中 Cd 质量比范围为0．06 mg/kg ～1．37 mg/kg，均值为0．23 mg/kg，与全国背景值相比，有一定程度富集；样品中 Cd 质量比成偏态分布，相对标准偏差较大。选用单项污染指数法对 Cd污染程度评价表明，镇江地区83％的土壤样品未受到 Cd 污染，14％为轻度污染，3％为中度污染。结合镇江地区的产业结构分析，电镀行业是土壤 Cd 污染的主要来源，道路运输、农药化肥在一定程度上也加重了污染。     

Can juvenile corals be surveyed effectively using digital photography?: implications for rapid assessment techniques

Seasonal variations in the concentrations of groundwater with respect to arsenic, lead, cadmium and aluminium has been studied in Dhemaji district of Assam, India. The water samples were collected from 20 different sites in both dry and wet seasons. The metals were analysed by using atomic absorption spectrometer, Perkin Elmer AAnalyst 200 model. The concentrations of aluminium, lead and cadmium in groundwater were found to be significantly elevated. High concentrations of all the metals were recorded in the dry season than in the wet season. Univariate statistics along with skewness, kurtosis and confidence limit have been calculated for both the seasons to test the distribution normality for each metal. Statistical analyses of the data reveal non-uniform distribution of the metals in the area. The metal contamination of groundwater in the district follows the trend Al > Pb > Cd > As in both the seasons.     

Use of multivariate indicator kriging methods for assessing groundwater contamination extents for irrigation

Multivariate geostatistical approaches have been applied extensively in characterizing risks and uncertainty of pollutant concentrations exceeding anthropogenic regulatory limits. Spatially delineating an extent of contamination potential is considerably critical for regional groundwater resources protection and utilization. This study used multivariate indicator kriging (MVIK) to determine spatial patterns of contamination extents in groundwater for irrigation and made a predicted comparison between two types of MVIK, including MVIK of multiplying indicator variables (MVIK-M) and of averaging indicator variables (MVIK-A). A cross-validation procedure was adopted to examine the performance of predicted errors, and various probability thresholds used to calculate ratios of declared pollution area to total area were explored for the two MVIK methods. The assessed results reveal that the northern and central aquifers have excellent groundwater quality for irrigation use. Results obtained through a cross-validation procedure indicate that MVIK-M is more robust than MVIK-A. Furthermore, a low ratio of declared pollution area to total area in MVIK-A may result in an unrealistic and unreliable probability used to determine extents of pollutants. Therefore, this study suggests using MVIK-M to probabilistically determine extents of pollutants in groundwater.