广东某含铊硫酸冶炼堆渣场土壤中重金属的污染特征

选取广东某硫酸厂工业堆渣周围土壤样品,重点研究了土壤剖面T1、cd、Pb、Zn四种重金属元素总量及形态分布特征.研究结果表明,该废渣在自然淋滤条件下已经对周围土壤产生了T1、Cd、Pb、Zn污染,并且T1、Pb、Cd较Zn污染严重.形态分析表明,堆渣场周围土壤中这些重金属主要是以残渣态和铁锰氧化物(氢氧化物)结合态存在.外围土壤受到的这些重金属污染及对环境的潜在危害大于废渣下伏土壤,其中在堆渣下伏土壤中主要以富集为主,而外围土壤中主要以迁移为主,且已经向土壤深处约30cm处进行了迁移.这些重金属污染物在表层土壤中未达到饱和状态,将继续在下伏土壤表层发生累积作用并且使横向土壤受污染的范围进一步扩大.     

某基岩区工业固体废物填埋场地递进式场地环境调查实例

针对某基岩区简易封场后的固体废物填埋场,采用多层次、递进式调查策略,配合使用地球物理探测、直压式土壤快速取样、现场快速检测等技术,分3个阶段开展填埋场及其周边环境调查。第1阶段,调查地质环境特征,开展地球物理探测;第2阶段,调查填埋物、渗滤液主要组分及对周边积水、农田土壤、民用井水的污染情况;第3阶段,划定重点污染区域,开展土壤和地下水污染调查。调查结果显示,填埋区已发生明显渗漏,对邻近区域土壤、地下水及地表积水造成了一定污染,但未对周边农用地土壤、民用井水质等产生不利影响,总体处于可控范围。提出,通过削减污染源,切断污染物迁移、暴露途径,消除已有污染影响,长期跟踪监测等多项管控治理措施进行综合整治。     

土壤重金属污染的工程危害及修复方法

分析了重金属污染对地基土和地下结构物的危害,比较了电动修复、土壤冲刷、原位土壤淋洗、化学固化修复土壤的优缺点,重点介绍固化/稳定化技术在修复重金属污染土壤中的应用。     

新疆土壤盐分的组成和分布特征

为了掌握监测区土壤盐分的组成和分布特征，通过采集监测样点地表0～30cm土层，对土壤总盐、八大离子等项目进行分析。结果表明，新疆土壤盐分含量高、盐分类型多样、盐分分布有一定的地带分布特性。同时土地利用方式的改变（人为活动）对土壤中盐分组成和分布有一定的影响。     

生物炭基缓释肥的制备及其对土壤理化性质的影响

通过淋溶试验分析生物炭热解温度、生物炭与尿素比例、粘结剂含量对生物炭基缓释肥缓释性能的影响,采用土壤培育试验研究生物炭基缓释肥对土壤理化性质的影响。结果表明,600 ℃下热解而成的生物炭缓释性能优于300 ℃下热解形成的生物炭;生物炭添加比例和粘结剂含量的增加能提升生物炭基缓释肥的缓释性能;生物炭基缓释肥的加入可降低培育土壤的容重,增大土壤的饱和导水率,提高土壤pH值和土壤有机质含量。     

基于PMF模型的矿区土壤重金属来源解析

通过在某矿区采集农田土壤和菠菜样品,分析其中重金属含量,基于相关性分析和PMF模型对该矿区农田土壤重金属来源进行解析。结果表明,研究区土壤中Cd、As、Zn、Cr和Cu 元素明显富集,分别是当地土壤背景值的5.7倍、4.4倍、2.4倍、1.5倍和1.3倍;相关性分析结果显示,研究区内Cu、Zn、As、Cd元素存在一定的相关性,可能具有同一污染源;PMF模型结果说明,研究区土壤中重金属主要来源分别为工业污染源、自然母质源、交通污染源和农业污染源,其对当地土壤重金属污染贡献率分别为39.8%、22.8%、21.6%和15.8%。     

XRF法检测土壤重金属的影响因素

对X射线荧光(XRF)法检测土壤重金属的影响因素进行探讨,研究证实土壤样品厚度、粒径和含水率均会对荧光强度产生影响,且影响程度与X射线的能量有关,对低能量X射线的影响显著大于对高能量X射线的影响。为保障分析的质量,在应用XRF法进行土壤重金属检测时,土壤样品应完全干燥,混合均匀,保持土壤粒径均匀一致,土壤样品厚度统一为10 mm。     

某金矿周边土壤和地下水中砷的健康风险评价

以湖北某含砷金矿污染场地为例,依据《污染场地风险评估技术导则》(HJ 25.3—2014),对其周边土壤和地下水中砷元素进行健康风险评价,结果表明:该金矿周边土壤和地下水中砷分别通过经口摄入土壤、皮肤接触土壤和吸入土壤颗粒物、饮用地下水4种暴露途径的致癌风险均超过可接受风险水平(10-6),对周边居民造成潜在危害。计算得到经口摄入、皮肤接触和吸入途径基于致癌效应的土壤风险控制值分别为1.6 mg/kg、9.3 mg/kg和12.1 mg/kg,应予以重视,并建议对矿山进行综合治理和目标值修复。     

重庆市菜地土壤和蔬菜中Hg、Pb的污染特征及相关性分析

通过对重庆市菜地土壤和蔬菜 Hg、Pb的含量分析 ,发现土壤 Hg含量远远大于背景值 ,并且土壤 Hg的含量与菜地周围的环境密切相关 ;土壤 Pb的含量同背景值相差不大。Hg、Pb在土壤和蔬菜中的污染特征表现为主城区 >近郊区 >远郊区 ;并且不同蔬菜品种中 Hg、Pb的含量差异较大 ,在不同蔬菜种类表现为叶菜类 >果菜类 >根菜类。相关性分析表明同一菜地土壤和蔬菜中 Hg、Pb含量无相关性 ;不同菜地土壤和蔬菜 Hg、Pb含量不具有相关性。     

土壤生态环境健康监测与评价技术现状与展望

综述了国内对土壤生态环境健康的研究进展,总结了传统土壤环境监测技术的不足,介绍了土壤生态环境健康监测技术,包括植物、动物、微生物等生态监测方法,旨在通过对各项技术的比较,了解各项监测技术对土壤健康监测和评价现状。对土壤生态环境健康监测与评价技术的发展趋势进行展望,提出未来需要对土壤生态健康监测技术进行标准化和定量化;开展多生物指标联合监测;结合遥感和物联网技术扩大土壤时空监测尺度,形成完整的土壤生态环境健康监测与评价体系,为环境管理部门有效监测土壤生态环境提供依据。     

常州市裸露地面风蚀扬尘排放清单及分布特征研究

以2014年为基准年,以常州市行政边界为研究区域,利用卫星遥感解译的土地利用类型和裸土面积信息,并通过国土、气象等部门提供的土壤类型、气象因子等相关资料获取本地化因子和参数,估算常州市行政区域内裸露地面土壤扬尘中颗粒物的年排放量。结果表明:常州市裸露地面主要分布在金坛市、溧阳市和武进区,市中心区域最少,裸露土地利用类型主要为农田、滩涂、裸露山体、荒地及未硬化或未绿化的空地等;2014年常州市行政区域内裸露地面风蚀扬尘中TSP、PM 10、PM 2.5的年排放量分别为62.66 t、5.63 t、0.24 t,其中,金坛市土壤起尘量最大,其次为武进区,再次为新北区、溧阳市,市中心区域土壤扬尘最少。     

中国北方干旱地区沙尘矿物特征研究

为了开展对我国沙暴传输规律的研究,了解我国北方干旱地区沙尘矿物特征有重要意义。本文对我国新疆塔克拉玛干沙漠区,内蒙腾格里沙漠区,贺兰山及银川等处的沙尘样品用X射线粉末衍射法进行矿物分析鉴定,并用原子吸收法作了特征元素的分析对比,根据矿物的X射线粉末衍射结果,结合元素分析,对沙漠源区及其以东地区沙尘矿物特征作了比较,判析了两个源区的矿物组成,讨论了它们的传输过程。     

西安市表层土壤和地表灰尘理化性质分析

以西安城市表层土壤和地表灰尘为研究对象,分析其基本理化指标。结果表明,西安市表层土壤pH值的变化范围是7.65~8.54,属弱碱性。地表灰尘pH值的变化范围是6.59~11.19,属碱性。表层土壤的低频磁化率和高频磁化率均值分别为1.55×10^-6 m^3/kg和1.46×10^-6 m^3/kg,频率磁化率均值为6.7%。地表灰尘的低频磁化率和高频磁化率均值分别为5.50×10^-6 m^3/kg和4.84×10^-6 m^3/kg,频率磁化率均值为1.88%。表层土壤和地表灰尘中总有机碳均值分别为1.31%和3.97%。西安城市表层土壤和地表灰尘均主要以粉粒为主,且二者各理化性质之间均有一定的相关性。     

碳酸盐碳测定在沙尘暴来源地识别中的应用

根据中国大气颗粒物特点 ,在国内沙尘暴研究中首次尝试利用碳酸盐碳进行沙尘暴来源地识别。测定了一系列黄沙、大气颗粒物和沙尘暴源区土壤样品。初步了解了上述样品中碳酸盐碳含量情况 ,结合国外研究结果对影响北京的沙尘暴源区进行推测并与其他方法作了比较     

Soil Contamination by Pb, Zn and Cn from a Lead Smeltery

In the environment of a lead smeltery contamination with lead, zinc and cadmium was measured over a 15-year period. Efficient bag filters were installed in order to remove dust from the flue gases. This measure of improvement resulted in a drastic reduction of lead, zinc and cadmium content in suspended particles (by 92, 94 and 89%), to a lesser extent in depositions (by 79, 75 and 68%), whereas in household dust the reduction was considerably lower (by 53, 55 and 70%). It can be assumed that household dust contains also redispersed soil particles on which the dust from the smeltery flue gases has deposited over years. To determine to what extent contaminated soil continues to cause increased population exposure directly or through plants or pastures, in the period 1981–1985 the content of metallic ions in the soil was measured at three depths. Selective solubility of soil metallic compounds was analysed in water, in 1 mol ammoniumacetate solution and in 0.05 mol ethylenediaminetetra-acetic acid (EDTA) solution in relation to their solubility in suspended particles, depositions and household dust. A considerably low portion of soluble metallic compounds was found in the soil and physico-chemical characteristics of the soil and portion of metallic ions bound to fulvice and humic acids were determined. The behaviour of metallic ions in contact with soil samples was studied in laboratory and it was found that approximately 50% of lead, 70% of zinc and 7% of cadmium ions change into non-soluble or poorly soluble compounds. By qualitative phase analysis in the non-soluble fraction PbO₂, Pb₃P₄O₁₃, Zn(OH)₂, ZnO, Fe₂O₃ and Cd(OH)₂ were identified.     

Northern Idaho House Dust and Soil Lead Levels Compared to the Bunker Hill Superfund Site

House dust has been identified as a major exposure medium for lead (Pb) in children. High levels of Pb in soil and house dust have been recorded at the Bunker Hill Superfund Site (BHSS) in northern Idaho, an historic mining and smelting district. Soil and dust remediation at the site was required; however, regional background soil and dust Pb levels had not been well characterized. The objective of this survey was to determine background house dust Pb levels and to compare those levels with concentrations, and dust and Pb loading rates measured at the BHSS. Soil and house dust samples were collected in five towns demographically similar to the BHSS but unaffected by the mining industry. The background concentrations and loading rates were significantly lower than those observed at the site. House age was a significant factor affecting background soil and house dust Pb concentrations and loading rates.     

淮南潘北矿塌陷湿地土壤退化评价

采煤带来的地面塌陷是极为重要的新生环境地质问题。以淮南潘北矿塌陷湿地为研究区域,其总氮(TN)含量平均水平为1.04g/kg,总磷(TP)含量平均水平为425mg/kg,在空间分布上均有从非季节性积水区向季节性积水区递减的趋势。土壤理化性质指标间总氮与有机质(SOM)含量呈极显著正向相关,与pH呈负向相关,与有效磷(AP)呈正向相关;总磷与有效磷表现为极显著相关;AP与有效钾(AK)、SOM都有很好的相关关系。通过应用相关分析和模糊数学的原理,以TN、TP、AP、AK和SOM等5个土壤肥力指标为基础,对该区域季节性积水区和非积水区土壤肥力进行数值化综合评价。季节性积水区IFI为0.463,非积水区IFI为 0.601,表明塌陷湿地形成后会加剧水域周边土壤的退化。     

全程加热采样管和半程加热采样管对超净排放污染源颗粒物监测结果的影响

根据《煤电节能减排升级与改造行动计划》以及《国家环境保护"十三五"规划纲要》,我国燃煤电厂污染物排放浓度应达到现行燃气锅炉标准,现行颗粒物监测仪器需要进行更新。现在市面上有2种污染源颗粒物采样管可对改造后电厂进行颗粒物采样监测,采用平行实验法对这2种采样管所采集的颗粒物质量结果进行分析,同时使用验证实验分析2种采样管颗粒物采集质量结果产生差异的原因,并对如何提升燃煤电厂颗粒物监测的准确性提出建议。     

Toxic effect caused on microflora of soil by pesticide picloram application

The toxic effect of the herbicide picloram on the microbial population of a typical Brazilian red Latosol soil was studied in a series of microcalorimetric experiments. The activity of the soil was stimulated by the addition of 6.0 mg of glucose and 6.0 mg of ammonium sulfate, under 34.8% controlled moisture, to a 1.50 mg soil sample, at 298.15 +/- 0.02 K. The net thermal effect due to the addition of the picloram to the soil was determined by interpreting the power-time curves, which were recorded on the microcalorimeter. The total thermal effect evolved by the microorganisms was affected by the increasing doses of herbicide, and varied from 0 to 10.00 micrograms g-1. An increase in picloram exposure caused a decrease of the original thermal effect, reaching a null value above 20.89 micrograms of herbicide per gram of soil. The decreases of the thermal effect evolved by microorganisms and the increase of the lag phase period are associated with the death of the microbial population. The effects caused by picloram application in this typical Brazilian soil resulted in a strong effect on the soil microbial communities.     

Use of zeolite to neutralise nickel in a soil environment

Nickel is a heavy metal which is a stable soil pollutant which is difficult to remediate. An attempt to reduce its impact on the environment can be made by changing its solubility. The right level of hydrogen ions and the content of mineral and organic colloids are crucial in this regard. Therefore, methods to neutralise heavy metals in soil are sought. There are no reports in the literature on the possibility of using minerals in the detoxication of a soil environment contaminated with metals. It is important to fill the gap in research on the effect of zeolites on the microbiological, biochemical and physicochemical properties of soils under pressure from heavy metals. Therefore, a pot experiment was conducted on two soils which examined the effect of various levels of contamination of soil with nickel on the activity of soil enzymes, physical and chemical properties and growth and development of plants. An alleviating effect of zeolite Bio.Zeo.S.01 on the negative impact of nickel on the soil and a plant (oats) was examined. The enzyme activity and the oat yield were found to be significantly and negatively affected by an excess of nickel in the soil, regardless of the soil type. The metal was accumulated more in the oat roots than in the above-ground parts. An addition of zeolite decreased the level of accumulation of nickel in oats grown only on sandy-silty loam. Zeolite Bio.Zeo.S.01 used in the study only slightly alleviated the negative effect of nickel on the biochemical properties of soil. Therefore, its usability in the remediation of soil contaminated with nickel is small.