用含硫化砷废渣制备砷酸铜

以湖北省某化工企业含砷废水处理过程中产生的含硫化砷废渣为研究对象,采用氧化碱浸—沉淀工艺制备砷酸铜。考察了沉淀反应液pH、沉淀反应温度、搅拌转速对砷沉淀效果的影响。采用XRD和SEM技术对砷酸铜的物相及形貌进行了表征。实验结果表明：废渣在氧化碱浸过程的砷浸出率为96.53%;沉淀反应时间为30 min时,沉淀步骤的最佳工艺条件为沉淀反应液pH 5.0、搅拌转速500 r/min、沉淀反应温度50 ℃。验证实验结果表明,在该工艺条件下,砷沉淀率均达93.96%以上。SEM表征结果显示,砷酸铜产品为颗粒状,粒径约为500 nm。XRD表征结果显示,砷酸铜产品中主要含有Cu₃As₂O₈,Cu₄O（AsO₄）₂,Cu₄（As₂O₇）O₂。该方法工艺简单、无二次污染,为废渣的综合利用提供了一种新的技术路线。     

锰矿浸渣中水溶性锰的回收

采用水洗—生石灰沉淀法回收锰矿浸渣中的水溶性锰,考察了液固比、水洗时间对锰矿浸渣中水溶性锰洗出率（洗出液与锰矿浸渣中水溶性锰的质量比）的影响,并探讨了n（生石灰）∶n（水溶性锰）、聚丙烯酰胺絮凝剂加入量、反应温度和反应时间对洗出液中水溶性锰回收率（沉淀与洗出液中锰的质量比）的影响。实验结果表明：水洗工段,在去离子水体积（mL）与锰矿浸渣质量（g）比为5∶1、水洗时间5 min的条件下,水溶性锰洗出率达到92%;生石灰沉淀工段,n（生石灰）∶n（水溶性锰）对水溶性锰回收率的影响最大,其次为反应温度、絮凝剂加入量和反应时间,在n（生石灰）∶n（水溶性锰）=1.8、絮凝剂加入量0.2 mg/L、常温、反应时间10 min的条件下,水溶性锰回收率达90%以上;锰矿浸渣中水溶性锰的总回收率达83%以上。     

Long‐Term Trends in Streamflow and Precipitation in Northwest California and Southwest Oregon, 1953‐2012

Using nonparametric Mann‐Kendall tests, we assessed long‐term (1953‐2012) trends in streamflow and precipitation in Northern California and Southern Oregon at 26 sites regulated by dams and 41 “unregulated” sites. Few (9%) sites had significant decreasing trends in annual precipitation, but September precipitation declined at 70% of sites. Site characteristics such as runoff type (groundwater, snow, or rain) and dam regulation influenced streamflow trends. Decreasing streamflow trends outnumbered increasing trends for most months except at regulated sites for May‐September. Summer (July‐September) streamflow declined at many sites, including 73% of unregulated sites in September. Applying a LOESS regression model of antecedent precipitation vs. average monthly streamflow, we evaluated the underlying streamflow trend caused by factors other than precipitation. Decreasing trends in precipitation‐adjusted streamflow substantially outnumbered increasing trends for most months. As with streamflow, groundwater‐dominated sites had a greater percent of declining trends in precipitation‐adjusted streamflow than other runoff types. The most pristine surface‐runoff‐dominated watersheds within the study area showed no decreases in precipitation‐adjusted streamflow during the summer months. These results suggest that streamflow decreases at other sites were likely due to more increased human withdrawals and vegetation changes than to climate factors other than precipitation quantity.     

基于集对分析的降水酸度及水质相似预测模型研究

应用集对分析法刻画历史样本之间的相似性,用多个最相似的历史样本的加权平均值作为当前样本预测值,建立了基于集对分析的降水酸度及水质相似预测模型(SFM-SPA),并运用该模型进行了降水酸度及水质预测的实例验证。结果表明,在主要影响因子选择适当、历史样本的代表性和相似性较好等限定条件下,利用模型进行环境预测是可行的,它较直观、计算简便,为环境污染预测提供了新的途径。     

络合沉淀—Fenton试剂氧化法处理高浓度含氰废水

采用络合沉淀—Fenton试剂氧化法处理高浓度含氰废水。实验结果表明,在初始废水p H为9、曝气时间为20 min、搅拌时间为20 min、Fe SO4溶液加入量为1.62 m L/L、搅拌转速为40 r/min的络合沉淀反应条件下,在絮凝阶段废水p H为8、n(H2O2)∶n(Fe2+)=20的Fenton试剂氧化反应条件下,处理初始CN-质量浓度为450~550 mg/L的高浓度含氰废水,总CN-去除率达99.9%以上,剩余CN-质量浓度小于0.02 mg/L,COD为50~70 mg/L,BOD5小于20 mg/L,浊度小于0.5 NTU,悬浮物质量浓度小于10 mg/L,满足GB 8978—1996《污水综合排放标准》的要求。     

超声辅助沉淀法制备γ-Bi_2MoO_6及其光催化性能

以Bi(NO3)3·5H2O和(NH4)6Mo7O24·4H2O为原料,采用超声辅助沉淀法制备了纳米可见光催化剂γ-Bi2Mo O6,用XRD,SEM,UV-Vis技术对其进行了表征,并以罗丹明B为目标降解物,考察了γ-Bi2Mo O6的可见光催化性能。表征结果显示,产物为高纯度正交结构的纳米γ-Bi2Mo O6,分散性良好。光催化实验结果表明:超声辅助沉淀法制备的γ-Bi2Mo O6的可见光催化活性优于普通沉淀法制备的产品;以超声辅助沉淀法制备的γ-Bi2Mo O6为光催化剂,在初始罗丹明B质量浓度为10 mg/L、初始溶液p H为7.2、γ-Bi2Mo O6加入量为10 g/L的最优条件下,反应180 min时的罗丹明B降解率达到97.48%。     

回收萘法苯酐生产废水中的富马酸

采用催化异构化、碱溶、脱色、酸析、过滤等工艺处理萘法苯酐生产废水,回收其中的富马酸。考察了碱的品种、碱溶pH、活性炭加入量、酸析pH等对富马酸产品外观质量和收率的影响。实验得到最佳工艺条件:采用氢氧化钠作为碱溶用碱,碱溶pH为6,活性炭加入量为0.5%(w),酸析pH为2。在此最佳工艺条件下制备的富马酸产品外观为白色,纯度达到99.1%,产品收率为72.8%。按30 kt/a苯酐生产装置计,每年可回收富马酸660 t,年利润429万元。     

Socio-economic vulnerability to climate change in the central mountainous region of eastern Mexico

Climate change effects are expected to be more severe for some segments of society than others. In Mexico, climate variability associated with climate change has important socio-economic and environmental impacts. From the central mountainous region of eastern Veracruz, Mexico, we analyzed data of total annual precipitation and mean annual temperature from 26 meteorological stations (1922–2008) and from General Circulation Models. We developed climate change scenarios based on the observed trends with projections to 2025, 2050, 2075, and 2100, finding considerable local climate changes with reductions in precipitation of over 700 mm and increases in temperature of ~9°C for the year 2100. Deforested areas located at windward were considered more vulnerable, representing potential risk for natural environments, local communities, and the main crops cultivated (sugarcane, coffee, and corn). Socio-economic vulnerability is exacerbated in areas where temperature increases and precipitation decreases.

Electronic supplementary material

The online version of this article (doi:10.1007/s13280-015-0690-4) contains supplementary material, which is available to authorized users.     

山西省大气降水水质评价

为了解山西省大气降水水质状况、主要污染物及区域分布规律，山西省水文部门于1984年开始对大气降水进行监测。在全省9个地市布设测点，分别为：太原市、大同市、长治市、榆次市、临汾市以及吕梁、忻州、阳泉、运城地区。监测项目为H^2 、电导率、Ca^2 、Mg^2 、K^2 、Na^2 、NH4^2 、SO4^2-、NO3^-、Cl^-、CO3^-、HCO3^-、F^-。结果表明，除吕梁、忻州地区外。山西省各地市均有酸雨发生，但酸雨发生的频率不高，全省年平均为3．3％；酸雨的酸性程度也不高，对生态可造成明显影响的降水次数不多；山西省酸雨为典型的硫酸型，酸雨中硫酸与硝酸的质量浓度比值远高于全国平均值。     

Spatial and Temporal Evaluation of Hydrological Response to Climate and Land Use Change in Three South Dakota Watersheds

This study analyzed changes in hydrology between two recent decades (1980s and 2010s) with the Soil and Water Assessment Tool (SWAT) in three representative watersheds in South Dakota: Bad River, Skunk Creek, and Upper Big Sioux River watersheds. Two SWAT models were created over two discrete time periods (1981‐1990 and 2005‐2014) for each watershed. National Land Cover Datasets 1992 and 2011 were, respectively, ingested into 1981‐1990 and 2005‐2014 models, along with corresponding weather data, to enable comparison of annual and seasonal runoff, soil water content, evapotranspiration (ET), water yield, and percolation between these two decades. Simulation results based on the calibrated models showed that surface runoff, soil water content, water yield, and percolation increased in all three watersheds. Elevated ET was also apparent, except in Skunk Creek watershed. Differences in annual water balance components appeared to follow changes in land use more closely than variation in precipitation amounts, although seasonal variation in precipitation was reflected in seasonal surface runoff. Subbasin‐scale spatial analyses revealed noticeable increases in water balance components mostly in downstream parts of Bad River and Skunk Creek watersheds, and the western part of Upper Big Sioux River watershed. Results presented in this study provide some insight into recent changes in hydrological processes in South Dakota watersheds. Editor's note: This paper is part of the featured series on SWAT Applications for Emerging Hydrologic and Water Quality Challenges. See the February 2017 issue for the introduction and background to the series.