准噶尔盆地南缘荒漠与农牧区交错带土壤Cu、Pb化学形态分布特征

采取Tessier连续提取法,研究了荒漠与农牧区交错带土壤中Cu,Pb的化学形态分布。结果表明,荒漠与农牧区交错带土壤中Cu、Pb主要以残渣晶格态为主,可交换态比例较低。Cu(荒漠土壤样品除外)的各形态含量之间的相互关系为:残渣态>有机物结合态>铁锰氧化物结合态>碳酸盐结合态>可交换态。荒漠土壤样品中重金属Cu各形态含量之间的相互关系为:残渣态>铁锰氧化物结合态>有机物结合态>碳酸盐结合态>可交换态;重金属Pb各形态含量之间的相互关系为:残渣态>铁锰氧化物结合态>碳酸盐结合态>可交换态>有机物结合态。重金属Pb的活性态较高,高于重金属Cu的活性态。     

生长于铬污染土壤上石榴产品铬污染评价

研究了攀西地区铬污染土壤和正常土壤铬含量分布及其石榴样品铬污染情况。结果表明攀枝花大田石榴基地土壤铬含量在23．1—504mg／kg，平均值高达184mg／kg，超标率为26％，而对该基地的石榴果实进行两年连续监测结果表明，铬含量在0．0012—0．067mg／kg之间，平均为0．016mg／kg，大大低于相应产品标准（0．5mg／kg），超标率为0％；会理石榴基地土壤铬含量在34．5—99．1mg／kg，平均值为69．0mg／kg，超标率为0％，该基地的石榴果实铬含量在0．0075—0．104mg／kg之间，平均为0．024mg／kg，大大低于相应产品标准（0．5mg／kg），超标率为0％。形态分析表明土壤中铬99％以上都是以不被植物利用的残渣态存在，因此土壤总铬再高，其被植物可吸收部分却很少，这就导致了受铬污染的土壤却不一定能生产出污染石榴的原因。     

不同粒径磷矿粉钝化土壤重金属Cd、Pb的机制研究

采用盆栽试验,研究磷矿粉不同粒径（0．1、1．5、150txm）的3种不同用量（1、2,4g·kg。土）钝化土壤重金属cd和Ph的效应及机制。结果表明,磷矿粉的粒径越小、用量越大,上海青产量越高,叶面积越大,植物体内cd、Pb的含量越低,土壤中交换态Cd、Pb的含量越低,残渣态cd、Pb的含量越高。与对照相比,0．1μm磷矿粉高用量（4g·kg-1土）的处理上海青的产量和叶面积分别显著增加87．3％和147．9％,叶中cd和Ph含量分别显著降低46．9％和61．9％,根中Cd和Pb含量分别显著降低47．9％和35.3％,土壤交换态cd和Ph含量分别降低44．8％和44．9％。150μm磷矿粉低用量（1g·kg-1土）处理叶面积、植物体内Cd、Pb含量与对照都没有达到显著差异。1．5μm磷矿粉处理效果介于0．1μm和150pm磷矿粉处理之间。可见,O．1μm磷矿粉钝化土壤重金属效果最好,其机制是降低了植物容易吸收的交换态cd和Pb的含量。     

土壤中钙、镁的形态分析及提取序列的研究

本文采用改进的BCR三步连续提取法对河北某食道癌高发地土壤中钙、镁进行了形态分析及提取序列的研究。实验表明：该地区土壤中镁主要以残渣态形式存在（占总量的83.66％-88.36％），钙则受提取序列的影响很大，在第一提取序列中，以酸溶态为主（74.11％-83.38％）；第二提取序列中，以有机物结合态为主（78.12％-97.17％）；第三、四提取序列中，以氧化物结合态为主（87.49％-103％）。提取剂的加入顺序明显影响到钙的各个形态的真实含量。     

我国3种自然土壤中Sb含量与化学形态分布特征研究

以重金属锑(Sb)为目标金属,研究潮土、黑土、和红壤中Sb含量,并利用元素富集率研究人类活动对土壤中Sb含量的影响,利用连续逐级提取法研究土壤中Sb的形态分布,探讨不同土壤中Sb活性特征。研究结果表明,Sb在潮土、黑土和红壤表层(0～30 cm)的含量分别为:1.76 mg/kg、1.24 mg/kg、3.44mg/kg,3种土壤中Sb富集率均小于2,研究区域Sb含量受人类活动扰动小;Sb主要赋存于残渣态、有机金属络合态、结晶氧化物结合态,Sb活性表现为:红壤>黑土>潮土。     

宜宾兴文县僰王山镇水田土壤中硒形态分布特征及研究

为了客观分析土壤中硒形态分布特征及硒有效性影响因素,依据硒不同形态下的溶解度不同,采用四步五态连续浸提取技术,由弱到强的选择顺序提取僰王山镇水田土壤中硒的水溶态、可交换态、有机质结合态、硫化物/硒化物态、残渣态这5种形态,并用原子荧光光谱法分析和氢化物发生-原子荧光光谱法测定了土壤样品中5种形态硒和总硒的含量。初步总结了研究区水田土壤硒含量特征和硒形态分布特征。研究结果发现,僰王山镇水田土壤总硒含量变化范围为0.51~0.93 mg/kg,平均值0.714 mg/kg,远远超过全国土壤总硒平均值0.290 mg/kg,且超过了目前认为的富硒土壤的标准值0.4 mg/kg。从土壤中5种形态分析结果所占比例来看,有机质结合态和硫化物/硒化物态硒是硒元素的主要赋存形态,两者占土壤总硒含量的54.63%,反应了研究区土壤中硒富集与有机质结合态存在密切关系。     

辽宁省污灌区土壤重金属铜、铬、镉和汞的形态研究

文章采用Tessier连续提取+AAS和AFS法对辽宁省污灌区土壤中铜、铬、镉和汞4种重金属的形态进行分析。研究结果表明,辽宁省污灌区土壤中重金属铜、铬、镉和汞的全部高于背景值。铜和铬的各形态分布趋势为:残渣态有机态铁锰氧化态碳酸盐态可交换态,镉的各形态分布趋势为:可交换态残渣态有机结合态铁锰氧化物结合态碳酸盐结合态,汞的各形态分布趋势为:残渣态有机态铁锰氧化态碳酸盐态可交换态,但可交换态、碳酸盐态和铁锰氧化态的Hg含量很低,所占比例可忽略为0。     

攀西地区主要蔬菜基地土壤重金属含量及评价

对攀西地区米易县蔬菜基地的土壤进行采样，用原子吸收和石墨炉光谱法分析土壤中Cr、Cu、Ni、Zn、Pb、Cd、As和Hg8种元素的含量。蔬菜基地土壤重金属平均含量分别为Cr 68．8mg／kg、Cu 22．3mg／kg、Ni27．6mg／kg、Zn 146．2mg／kg、Pb31．7mg／kg、Cd0．258mg／kg、As10．3mg／kg、Hg0．0618mg／kg。根据土壤环境质量标准（GB15618—1995）对检测结果进行了单因子和多因子综合污染指数评价。分析表明调查区内少部分蔬菜基地土壤受到轻度重金属污染，主要污染物为Cd元素，其余重金属元素的含量均在安全警戒线内。     

土壤镉处理对棉花镉吸收及分布规律的影响

用CdCl2将盆栽土壤Cd浓度处理为1mg／kg、5mg／kg、10mg／kg、20mg,／kg、30mg／kg种植棉花，研究棉花对镉的吸收及镉在棉花体内的分布规律。结果表明，当土壤镉浓度小于30mg／kg时，镉在棉花体内的分布呈现不同的规律。当土壤镉浓度小于5mg／kg时，镉主要分布在棉花的地上部；当土壤镉浓度大于20mg／kg时，镉主要分布在棉花的叶片、根、茎中，其中叶片的镉含量最高，棉絮镉含量最低。不同镉污染水平下，棉花的镉富集系数均小于1。当土壤镉污染浓度为5mg／kg时，棉花叶片的镉富集系数为0．76。在同一镉污染水平下，棉花叶片的镉转运系数最高。当土壤镉含量小于20mg／kg时，棉花茎、叶、棉絮的转运系数平均为4．63。     

攀枝花市攀钢工业区土壤重金属污染特征及评价

本文对攀枝花市攀钢工业区土壤中五种重金属元素（Cu、Pb、Zn、Cr、Cd）的空间的分布特征、形态分布特征进行了研究，并应用污染负荷指数法对各重金属的污染程度进行了评价。研究发现，Cu、Pb、Zn、Cr的最大值与最小值分别相差2．98、3．4、5．2、2．7倍，cd的最大值与最小值甚至相差15．7倍。重金属元素相关性特征可分为Cd—Pb—Zn和Cu—Cr两组。形态分布特征表现在Cu、Zn、Pb、Cr主要以稳定的残渣态存在，Cd主要以可利用性最强的可交换态和碳酸盐结合态存在。污染较严重的是攀钢机关、攀钢原料场。     

Uptake and distribution of iodine in rice plants

Rice (Oryza sativa L.) plants were cultivated in an experimental field and separated at harvest into different components, including polished rice, rice bran, hull, straw, and root. The contents of iodine in these components and the soil were determined by inductively coupled plasma-mass spectrometry and radiochemical neutron activation analysis, respectively. Iodine content varied by more than three orders of magnitude among the plant components. Mean concentration of iodine in the entire plants was 20 mg kg(-1) dry weight, and the concentration of iodine in the surface soil (0-20 cm depth) was 48 mg kg(-1). The highest concentration of iodine (53 mg kg(-1) dry weight) was measured in root and the lowest concentration (0.034 mg kg(-1) dry weight) in polished rice. While the edible component (polished rice) accounted for 32% of the total dry weight, it contained only 0.055% of iodine found in the entire rice plants. Atmospheric gaseous iodine (5.9 ng m(-3)) was estimated to contribute <0.2% of the total iodine content in the biomass of rice plants; therefore nearly all of the iodine in the rice plants was a result of the uptake of iodine from the soil. The content of iodine in the aboveground part of rice plants was 16 mg kg(-1) dry weight and the percentage of iodine transferred per cropping from the soil into the aboveground biomass corresponded to 0.27% (20 mg m(-2)) of the upper soil layer content.     

Lead phytoextraction from contaminated soil with high-biomass plant species

In this study, cabbage [Brassica rapa L. subsp. chinensis (L.) Hanelt cv. Xinza No 1], mung bean [Vigna radiata (L.) R. Wilczek var. radiata cv. VC-3762], and wheat (Triticum aestivum L. cv. Altas 66) were grown in Pb-contaminated soils. Application of ethylenediaminetetraacetic acid (EDTA) (3.0 mmol of EDTA/kg soil) to the soil significantly increased the concentrations of Pb in the shoots and roots of all the plants. Lead concentrations in the cabbage shoots reached 5010 and 4620 mg/kg dry matter on Days 7 and 14 after EDTA application, respectively. EDTA was the best in solubilizing soil-bound Pb and enhancing Pb accumulation in the cabbage shoots among various chelates (EDTA, diethylenetriaminepentaacetic acid [DTPA], hydroxyethylenediaminetriacetic acid [HEDTA], nitrilotriacetic acid [NTA], and citric acid). Results of the sequential chemical extraction of soil samples showed that the Pb concentrations in the carbonate-specifically adsorbed and Fe-Mn oxide phases were significantly decreased after EDTA treatment. The results indicated that EDTA solubilized Pb mainly from these two phases in the soil. The relative efficiency of EDTA enhancing Pb accumulation in shoots (defined as the ratio of shoot Pb concentration to EDTA concentration applied) was highest when 1.5 or 3.0 mmol EDTA/kg soil was used. Application of EDTA in three separate doses was most effective in enhancing the accumulation of Pb in cabbage shoots and decreased mobility of Pb in soil compared with one- and two-dose application methods. This approach could help to minimize the amount of chelate applied in the field and to reduce the potential risk of soluble Pb movement into ground water.     

Chemical immobilization of lead, zinc, and cadmium in smelter-contaminated soils using biosolids and rock phosphate

Chemical immobilization, an in situ remediation method where inexpensive chemicals are used to reduce contaminant solubility in contaminated soil, has gained attention. We investigated the effectiveness of lime-stabilized biosolid (LSB), N-Viro Soil (NV), rock phosphate (RP), and anaerobic biosolid (AB) to reduce extractability and plant and gastrointestinal (GI) bioavailability in three Cd-, Pb-, and Zn-contaminated soils from smelter sites. Treated (100 g kg(-1) soil) and control soils were incubated at 27 degrees C and -0.033 MPa (0.33 bar) water content for 90 d. The effect of soil treatment on metal extractability was evaluated by sequential extraction, on phytoavailability by a lettuce bioassay (Lactuca sativa L.), on human GI availability of Pb from soil ingestion by the Physiologically Based Extraction Test. The largest reductions in metal extractability and phytoavailability were from alkaline organic treatments (LSB and NV). Phytotoxic Zn [1188 mg Zn kg(-1) extracted with 0.5 M Ca(NO3)2] in Blackwell soil (disturbed soil) was reduced by LSB, NV, and RP to 166, 25, and 784 mg Zn kg(-1), respectively. Rock phosphate was the only treatment that reduced GI-available Pb in both gastric and intestinal solutions, 23 and 92%, respectively. Alkaline organic treatments (LSB, NV) decreases Cd transmission through the food chain pathway, whereas rock phosphate decreases risk from exposure to Pb via the soil ingestion pathway. Alkaline organic treatments can reduce human exposure to Cd and Pb by reducing Zn phytotoxicity and revegetation of contaminated sites.     

Weathering of lead bullets and their environmental effects at outdoor shooting ranges

Lead contamination at shooting range soils is of great environmental concern. This study focused on weathering of lead bullets and its effect on the environment at five outdoor shooting ranges in Florida, USA. Soil, plant, and water samples were collected from the ranges and analyzed for total Pb and/or toxicity characteristic leaching procedure (TCLP) Pb. Selected bullet and berm soil samples were mineralogically analyzed with X-ray diffraction and scanning electron microscopy. Hydrocerussite [Pb3(CO3)2(OH)2] was found in both the weathered crusts and berm soils in the shooting ranges with alkaline soil pH. For those shooting ranges with acidic soil pH, hydrocerussite, cerussite (PbCO3), and small amount of massicot (PbO) were predominantly present in the weathered crusts, but no lead carbonate mineral was found in the soils. However, hydroxypyromorphite [(Pb10(PO4)6(OH)2] was formed in a P-rich acidic soil, indicating that hydroxypyromorphite can be a stable mineral in P-rich shooting range soil. Total Pb and TCLP Pb in the soils from all five shooting ranges were significantly elevated with the highest total Pb concentration of 1.27 to 4.84% (w/w) in berm soils. Lead concentrations in most sampled soils exceeded the USEPA's critical level of 400 mg Pb kg(-1) soil. Lead was not detected in subsurface soils in most ranges except for one, where elevated Pb up to 522 mg kg(-1) was observed in the subsurface, possibly due to enhanced solubilization of organic Pb complexes at alkaline soil pH. Elevated total Pb concentrations in bermudagrass [Cynodon dactylon (L.) Pers.] (up to 806 mg kg(-1) in the aboveground parts) and in surface water (up to 289 microg L(-1)) were observed in some ranges. Ranges with high P content or high cation exchange capacity showed lower Pb mobility. Our research clearly demonstrates the importance of properly managing shooting ranges to minimize adverse effects of Pb on the environment.     

TCLP法评价钢铁工业区周边土壤重金属生态环境风险

采用土壤随机布点法,采集某钢铁工业区周边34个土壤样品,利用美国TCLP法对钢铁工业区周边土壤重金属（Cu、 Zn、 Pb、 Cd）有效态进行实验分析和生态风险评价。结果表明, Cu、 Zn、 Pb、 Cd有效态含量分别在0.87~57.7 mg/kg、5.20~1338 mg/kg、1.09~379 mg/kg、1.15×10-3~69.9×10-3 mg/kg之间,钢铁工业区土壤不同程度地受到重金属的污染,其中以Zn污染最为严重。内梅罗污染指数评价中,处于安全水平的点位仅占17.6%,受到污染的点位占55.9%。其中,轻污染占20.6%,中污染占2.9%,重污染占32.4%。     

Analysis of heavy metals and aromatics compounds in soil layers of a sanitary landfill

Solid waste presents the potential for contamination of the soil when it is improperly managed. One of the great challenges of today's society is to promote the proper disposal of municipal solid waste in order to guarantee the safety of public health and to avoid risks to the environment. In this context, the objective of this study is to analyze the concentration profiles of heavy metals and aromatic hydrocarbons of risk that human health in landfill soil. Such works provides an important tool to evaluate the possible presence of contaminants from inappropriate waste disposal, as well as to assist in the management of waste and to prevent environmental contamination. In order to analyze cadmium (Cd), lead (Pb), nickel (Ni), arsenic (As), and mercury (Hg), which are toxic elements, and aromatic hydrocarbons, including benzene, toluene, ethylbenzene, o‐xylene, m‐xylene, and p‐xylene, soil samples were collected at different sites and depths. Neither Cd nor As was detected in any of the samples that were analyzed. Pb levels ranged from 5.34 milligrams per kilograms (mg/kg) to 7.40 mg/kg, Ni levels ranged from 2.17 mg/kg to 3.00 mg/kg, and Hg levels ranged from 75.4 micrograms per kilograms (μg/kg) to 88.3 μg/kg. The aromatic hydrocarbon compounds of benzene, toluene, ethylbenzene, and o‐xylene were below 5.5 μg/kg, and m‐, p‐xylene was below 11 μg/kg. The analysis of heavy metals and aromatic hydrocarbons present in the landfill soil showed concentrations below the soil quality guideline values of the Brazilian National Environment Council (CONAMA) Resolution 420, which has criteria for the presence of chemical substances in soil for Brazil. Therefore, the low levels of chemicals may be related to the operational time of the landfill or to the population profile of the municipality, which is predominantly composed of persons involved in family‐based agriculture.     

西湖和东苕溪沉积物重金属化学形态分析

不同赋存形态重金属的环境行为和生态效应不同,水体沉积物中重金属的迁移转化及其潜在环境危害更大程度上取决于其赋存形态。本研究在西湖和东苕溪设置12个采样点采集沉积物样品,采用改进BCR分步提取法,提取了重金属污染物的4种化学形态,分别为弱酸提取态、可还原态、可氧化态及残渣态。结果表明:沉积物中Cd以弱酸提取态为主,对外界环境的变化极其敏感,并易于发生迁移转化,生态风险较高。Cu离子对有机质表现出极强的亲和力导致Cu的可氧化态含量较高也有一定的生态风险。Pb会被Fe-Mn氧化物所吸附导致Pb的可还原态含量较高,存在较高的潜在生态危害。Mn的弱酸提取态、可还原态和残渣态含量都较高,在迁移的过程中变化地较快,能够逐渐降低Mn对自然环境的危害。其他各重金属(As、Cr、Zn)则都以残渣态为主,潜在危害较低。     

Heavy metals distribution in an Iowa suburban landscape

This study investigated the degree to which human activities through urbanization influence heavy metal concentrations in a suburban landscape in Ankeny, IA. Residential areas from different years in nine time periods of development were identified from aerial photos. Soil cores were collected from the center of the front yard of 10 randomly selected homes. Cores were subdivided into 0- to 5-, 5- to 10-, and 10- to 20-cm increments from a composite of five cores. The soils were analyzed for organic C, pH, and total Cd, Co, Cr, Cu, Ni, Pb, and Zn. Results showed that organic C increased and pH decreased with time, and that there was a general decreasing trend in heavy metal concentrations from the pre-1939 period until 1983-1990, after which there was a sharp increase in the concentrations of most of the metals. The mean Cu concentration ranged from 21 mg kg(-1) for the pre-1939 time period of development to 14.9 mg kg(-1) for the recent period of development (2003-2005). Nickel concentrations increased significantly with depth with means of 21.3 mg kg(-1) at depth 0 to 5 cm, 22.5 mg kg(-1) at depth 5 to 10 cm, and 23.0 mg kg(-1) at depth 10 to 20 cm. The concentrations of heavy metals were significantly intercorrelated, except Zn, suggesting their coexistence as mineral constituents or common contamination source. The concentrations of Cu and Pb in some locations could be due to anthropogenic inputs or higher organic matter content in soils adjacent to older homes. There appears to have been a source that caused an increase in Cd, Cr, Co, Cu, Pb, and Ni concentrations in soil adjacent to homes built between 1983 and 1990.