Effects of Groundwater-Flow Paths On Nitrate Concentrations Across Two Riparian Forest Corridors1

Speiran, Gary K., 2010. Effects of Groundwater-Flow Paths on Nitrate Concentrations Across Two Riparian Forest Corridors. Journal of the American Water Resources Association (JAWRA) 46(2):246-260. DOI: 10.1111/j.1752-1688.2010.00427.x Abstract: Groundwater levels, apparent age, and chemistry from field sites and groundwater-flow modeling of hypothetical aquifers collectively indicate that groundwater-flow paths contribute to differences in nitrate concentrations across riparian corridors. At sites in Virginia (one coastal and one Piedmont), lowland forested wetlands separate upland fields from nearby surface waters (an estuary and a stream). At the coastal site, nitrate concentrations near the water table decreased from more than 10 mg/l beneath fields to 2 mg/l beneath a riparian forest buffer because recharge through the buffer forced water with concentrations greater than 5 mg/l to flow deeper beneath the buffer. Diurnal changes in groundwater levels up to 0.25 meters at the coastal site reflect flow from the water table into unsaturated soil where roots remove water and nitrate dissolved in it. Decreases in aquifer thickness caused by declines in the water table and decreases in horizontal hydraulic gradients from the uplands to the wetlands indicate that more than 95% of the groundwater discharged to the wetlands. Such discharge through organic soil can reduce nitrate concentrations by denitrification. Model simulations are consistent with field results, showing downward flow approaching toe slopes and surface waters to which groundwater discharges. These effects show the importance of buffer placement over use of fixed-width, streamside buffers to control nitrate concentrations.     

测定单个粒子的薄膜法及其应用

本文介绍改进后的薄膜法,主要是形态分析法和复合薄膜法。它们都是基于粒子和薄膜反应生成物的形态特征通过电镜来确定粒子成分的。前者可以检测单个酸性粒子,检出下限为７ ×１０－ １９ｇ;后者能同时检出一个粒子中所含的ＮＯ－３ 和ＳＯ２ －４ ,检出下限分别为３ ×１０－ １５ｇ 和７ ×１０－ １８ｇ。利用该方法对广州大气粒子进行了观察,结果表明改进后的薄膜法完全适用于对单个粒子的观察和测定。     

氢气还原海绵铁去除水体中硝酸盐的研究

利用小球烧结和氢气还原工艺制备了粒径1mm～5mm的多孔性球形海绵铁,对球形海绵铁去除水体中硝酸盐的效率及去除动力学进行了研究。结果表明:溶液初始pH值对硝酸盐去除效率的影响显著,初始pH值小于3时,硝酸盐的去除率随溶液初始pH的增加而逐渐降低;初始pH值大于3时,硝酸盐的去除率又随之升高。硝酸盐浓度低于10mgN/L时,硝酸盐去除率随着硝酸盐初始浓度的增加而增加,硝酸盐的残余量保持在0.4mgN/L左右;硝酸盐浓度高于20mgN/L时,硝酸盐的去除率随初始硝酸盐浓度的增加而略有降低。球形海绵铁去除硝酸盐为一级动力学反应,反应级数为0.970～1.378,表观反应速率常数为0.314h-1～0.536h-1。海绵铁还原硝酸盐的主要产物为氨氮,随着还原反应的进行,溶液pH值快速增加,氨氮以分子态氨的形式从水中逸出。进行归纳总结和对比,并以多环芳烃的提取为例列举了各方法的应用步骤,从而为其他环境样品其他有机物分析预处理提供参考。     

稀土钇对蚯蚓的急性毒性及蚓体内蓄积研究

文章以蚯蚓为指示生物,分别采用滤纸接触法和自然土壤法研究了稀土元素钇对蚯蚓的急性毒性效应。结果表明,滤纸接触法测得钇对蚯蚓的半数致死浓度LC50为0.18 g/L;土壤法所测LC50值为1.08 g/kg。可见,稀土钇对蚯蚓具有毒性作用,但属低毒级,并且自然土壤法中蚯蚓的半数致死浓度要低于滤纸接触法中的结果。应用ICP-AES分别研究了2种实验方法中钇在蚯蚓体内的富集情况,发现硝酸钇浓度及染毒时间、蚯蚓的死亡率及速度和钇在蚯蚓体内的富集三者存在显著的相关性。     

聚合磷硫酸铁富集铬(Ⅵ)的研究

阐述了新型无机吸附共沉淀剂——聚合磷硫酸铁对废水中铬的富集的研究情况,以铬(Ⅵ)的去除率为参数,确定了聚合磷硫酸铁用量、温度、pH值及铬含量等因素的影响。实验表明该絮凝剂能有效地分离废水中的铬,使处理后水质指标符合国家排放标准。     

新型聚硅氯化铁铝絮凝剂的制备及性能

以二甲基二氯硅烷为硅源,与氯化铁、氯化铝聚合制得新型的聚硅氯化铁铝（PSFAC）絮凝剂,考察了制备条件及PSFAC对含油废水和药厂废水的絮凝效果。制备PSFAC的最佳条件：nFc：nAl为0．4,nSi：n（Al＋Fe）为0．1,碱化度为2．0,C（Al,Fe）、为0．1mol／L,熟化时间为1-2d。当PSFAC加入量为10mg／L时,对含油废水、药厂废水的浊度去除率分别为84％和86％。PSFAC具有加入量少、沉降速度快、适用的pH范围较宽等优点。     

不同磁黄铁矿自养反硝化脱氮除磷作用

氮磷排放标准日趋严格,开发高效廉价脱氮除磷材料已成为研究热点.采用黄铁矿与赤铁矿在管式炉中氮气气氛下600 ℃煅烧,得到硫化赤铁矿形成的磁黄铁矿、黄铁矿热分解形成的磁黄铁矿,构建磁黄铁矿-方解石体系处理含氮磷模拟废水,对比不同方式制备的磁黄铁矿、天然磁黄铁矿、黄铁矿、硫磺脱氮除磷性能,考察不同磁黄铁矿晶体结构和结晶度差异及其对脱氮除磷影响,探究不同体系中矿物结构和微生物群落变化.结果表明：黄铁矿热分解产物以六方磁黄铁矿为主;硫化赤铁矿产物以低结晶度的单斜磁黄铁矿为主,因而表现出优异的脱氮除磷活性,氮磷去除率分别为99.8%和96.8%.铁硫化物与微生物反应产物的XRD、SEM和FE-TEM分析结果表明,微生物能有效利用磁黄铁矿进行脱氮,磷酸盐主要以FePO₄形式被去除.群落分析结果表明铁硫化物脱氮除磷体系中的主要功能菌属为Thiobacillus和 Sulfurimonas,结晶度低的单斜磁黄铁矿更有利于Thiobacillus定向富集.