广西桂东北地区农业土壤环境若干重金属元素背景值的调查

应用分层抽样统计方法,调查研究广西桂东北地区农业土壤环境Cu、Zn、Pb、Cd、Ni、As、Cr、Hg等8种重金属元素背景值,并分别求算出各元素背景值95％的置信区间。经方差分析,各成土母质间几种元素背景值都有不同程度差异。探讨了该区域农业土壤元素背景值与世界土壤、地壳丰度和国内土壤元素背景值的差异,为开展农业环境科学研究提供依据。     

山西省五台山区土壤氟元素的环境背景值及分布规律

对山西省五台山区垂直土壤主要土类的氟元素背景值进行了调查与分析，揭示了五台山区土壤氟元素区域背景的分布特征和变化趋势。结果表明：五台山区土壤氟背景值略高于我国平均水平，多数土壤Ｂ层含氟量最高。     

山西省五台山区土壤氟元素的环境背景值及分布规律

对山西省五台山区垂直土壤主要土类的氟元素背景值进行了调查与分析，揭示了五台山区土壤氟元素区域背景的分布特征和变化趋势。结果表明：五台山区土壤氟背景值略高于我国平均水平，多数土壤Ｂ层含氟量最高。     

天津南港工业区土壤环境背景值调查

通过对天津南港工业区土壤环境背景值的调查研究,对其土壤进行了环境质量评价,并得出了该区域土壤元素的分布规律。在与其他地区的土壤背景值进行比较后,指出了其异同点。天津南港工业区土壤元素在垂直方向上以不规则分布型为主,但As和Cd在土壤表层和深层的含量变化差异较小,Pb表现为表层富集。水平方向上,园区西北部的土壤元素含量比...     

佛山城市森林公园表层土壤重金属累积特征、影响因素及其评价

研究区域经济快速发展对城市森林生态系统影响,明确城市森林公园土壤重金属污染程度,可为城市森林公园土壤管理和城市土壤安全利用与保护提供理论依据。以佛山市城市森林公园林区为研究对象,依据其分布格局随机选取11个林区,分析了样地土壤中8种重金属(Cd、Pb、Cr、Cu、Ni、Zn、Hg、As)累积特征,通过单因子评价指标进行评价及影响因素分析。结果表明,(1)佛山市城市森林公园表层土壤重金属环境质量整体良好,不同样地质量分数差异较大,其中重金属Ni元素质量分数均值略超珠三角背景值,其余重金属元素质量分数均值都低于珠江三角洲背景值,均不构成人身接触健康风险。(2)佛山城市森林公园土壤重金属主要受森林土壤成土过程及干湿沉降影响,其次为林业管理和汽车燃油。(3)中央公园样地8种重金属均低于背景值,其余样地均有不同重金属、不同程度超出珠三角土壤重金属环境背景值,其中Ni在王借岗公园、As在西樵山公园分别是区域背景值的4.34倍和3.80倍,达到重污染级别;Pb在李小龙乐园、As在大南山林场是区域背景值2.28倍和2.09倍,达到中度污染级别,各影响因素叠加累积效应可能是导致土壤重金属超出背景值的种类多和强度大的原因。(4)佛山城市森林公园11个样地中,超出珠三角土壤背景值频度最高的为Cr元素,其次为As元素,其中王借岗公园样地Cd、Cr、Cu、Zn、Ni超出区域背景值;西樵山公园样地Hg、Zn、As超出区域背景值;李小龙乐园样地、大南山公园样地、桫椤保护区样地和佛山植物园样地均有2种重金属超出区域背景值,其余样地为单元素超出区域背景值或没有重金属超出区域背景值。     

三峡库区消落带土壤中铅污染调查

报道了三峡库区长江干流及小江支流消落带土壤中重金属铅含量背景值的调查结果。结果表明，目前土壤未被重金属铅污染。     

内蒙古典型草原土壤的氟含量

对内蒙古草原区典型草原不同区域内土壤氟水平及分布规律进行了研究。结果表明，典型草原土壤氟含量从东到西呈上升趋势，典型草原土壤表层氟含量平均值为２８５．４６ｍｇ／ｋｇ，与国内外有关文献值相比属中等水平，处于内蒙古土壤表层氟背景值范围内。     

内蒙阿拉善地区植物与土壤元素背景值特征及其相互关系

内蒙阿拉善地区植物、土壤的元素背景特征及其相互关系的研究结果表明：５３种植物的９种元素（Ｚｎ、Ｃｕ、Ｎｉ、Ｐｂ、Ｃｄ、Ｃｏ、Ｃｒ、Ｖ、Ｍｎ）背景含量有很大差异．不同生活型植物背景值也各异，总的规律为：Ｍｎ＞Ｚｎ＞Ｖ＞Ｃｕ＞Ｎｉ＞Ｃｒ＞Ｐｂ＞Ｃｏ＞Ｃｄ；同种植物的元素含量在不同群落中有明显差别，但都在同一个数量级．土壤９种元素的背景含量均以Ｍｎ含量最高，其次为Ｚｎ和Ｖ，Ｃｄ的含量最低；不同上类各剖面各种元素的垂直分布规律为底层或表层的元素含量高于中间各层．土壤元素背景值都高于植物背景值，前者一般为后者的２～２０倍．植物对元素的吸收系数以Ｃｄ最大，Ｃｒ最小．土壤元素含量与有机质含量的相关性因土类不同而异：沙土的有机质含量最低，只有Ｚｎ含量与有机质相关性显著；而盐土的有机质含量最高，有Ｃｏ、Ｃｄ、Ｍｎ、Ｎｉ、Ｃｒ、Ｚｎ６种元素含量与之显著相关．     

内蒙古典型草原土壤的氟含量

对内蒙古草原区典型草原不同区域内土壤氟水平及分布规律进行了研究。结果表明，典型草原土壤氟含量从东到西呈上升趋势。典型草原土壤表层氟含量平均值为２８５．４６ｍｇ／ｋｇ，与国内外有关文献值相比属中等水平，处于内蒙古土壤表层氟背景值范围内。     

土壤元素背景值影响因素的剖析

土壤元素背景值影响因素的研究是环境背景值研究的一项重要课题,在野外工作基础上应用主组元分析及聚类分析两者结合的方法,研究影响土壤元素的各种因素,是一种行之有效的方法。本文使用这种方法研究了影响江苏省一些土壤元素背景值的因素,并根据各自所受的主要影响进行了分类。可分为综合作用影响型、火成岩母质影响型、海成沉积岩母质影响型、现代表生作用影响型,并得到一组计算未知类型的主组元方程,用以估测影响这些未知类型土壤元素背景值的主要因素。     

燃煤灰渣中微量元素分布规律的研究

研究了锅炉飞灰和底灰中１５种微量元素的含量和分布，探讨了煤炭燃烧后，微量元素在灰渣中的集散及其影响因素，飞灰和底灰中大多数元素高于全国土壤背景值，７种元素高于克拉克值，其余８种低于克拉克值，飞灰中多数元素的地球化学富集因子高于１，呈富集状态，而底灰中多数元素富集因子小于１，飞灰和底灰中微量元素含量与煤中微量元素含量呈线性关系，微量元素含量不仅与煤有关，还受锅炉燃烧方式等人为因素影响。     

东北、内蒙古东部地区煤炭中微量元素含量及分布规律

研究了东北和内蒙东部各矿区煤炭中As,Ba,Be,Cb,Co,Cr,Cu,Hg,Li,Mn,Ni,Pb,Se,Sr,V,Zn,Zr的含量水平及分布规律.煤灰灰分中多数元素含量高于克拉克值、土壤背景值及植物干物质中含量,呈富集状态.相关矩阵和聚类分析表明,煤炭中微量元素含量与基质元素有密切的依存性.由于复杂的成煤过程,煤炭中微量元素呈现独特的集散规律.     

Background levels of microelements in soils of Italy

A systematic survey on the distribution of geochemically and texicologically relevant trace elements in the soils of Italy was carried out on 32 soil profiles, developed in different environmental and pedological conditions. The aim of this study was to collect basic information on the background levels of trace elements, their geochemical behaviour and the relationships between weathering and pedogenetic processes. The statistically processed analytical results led to the following conclusions: (i) Trace element distribution in the profiles studied is consistent with pedochemical behaviour and rock lithology. A comparison with the world soil means shows that there are no significant differences, except for those elements largely utilised in agriculture (Cu, Zn) or, because of pollution, (Pd, Cd), or natural accumulation (Ni, Cr); (ii) data processing by cluster analysis shows marked correlations between some elements, for example, Al-V, Ni-Cr, Mn-Co. Groups of geochemically homogeneous samples, which correspond to the great soil families characteristic of each pedological landscape, are also indicated; (iii) evidence of soil contamination is provided by the high levels of some elements, especially in the A horizon. Cu and Zn seem to be concentrated in the Ap horizon of cultivated soils, while Pd and Cd may be derived from the atmosphere.     

西安东郊某废弃钢铁厂油松年轮记录的重金属含量变化过程

以西安市东郊某废弃钢铁厂为例,采用石墨炉原子吸收法、电感耦合等离子体原子发射光谱法、原子荧光法测定了废弃钢铁厂两棵油松(Pinus tabulaeformis Carr.)树盘及其根部土壤中重金属Cr、Mn、Hg、Zn、Pb、Cd和类金属As以及P等8种元素的含量.土壤测定结果表明,该地区Cr、Zn、As等元素含量超过了西安市郊区土壤背景值,Cr、Mn等元素易在深层土壤中积累,Hg、Zn等元素不易在深层土壤中积累.两个树盘年轮中这8种元素的含量随着年代的推移总体呈现上升的趋势,这表明该地区由这些元素引起的污染状况日益加重.Hg、Pb、Cd等元素于1996年左右吸收达到最高峰,与该钢铁厂生产历史相一致.这两个树盘中Mn、Hg、Zn、As、P等元素自1993年后均呈现比较一致的增长趋势.通过计算各元素的自相关系数,从统计学角度发现这8种元素在油松年轮中的迁移特征:Mn、Zn、As等元素均存在着3年的横向迁移趋势,Pb、P存在2年的迁移趋势,Hg、Cd有1年的迁移,而Cr几乎不迁移,其中Zn、Cd、P等元素在油松中的迁移趋势与西安市西部某地区椿树和桐树中的迁移趋势表现一致.     

Assessing the effect of long-term crop cultivation on distribution of Cd in the root zone

Trace elements such as cadmium (Cd) may be inadvertently added to cropland soils through application of fertilizers, irrigation water, and other amendments. These toxic trace elements pose a potentially threat to soil quality and, through the food chain transfer, to human health. A generalized soil trace element mass balance model that accounts for the interactive processes governing the reactions of trace elements in soils, and consequently removed with crop harvest and leaching out of the soil profile with irrigation water was developed in this research. The model conceptually approximates the mechanisms and kinetics of a real field cropland system. The model was used to evaluate the long-term cultivation on distribution of Cd in California croplands. Under typical California cropping practices, Cd added into the soils accumulated primarily in the plow layer while the Cd content below the plow layer was barely affected. After 100 years of continuous cultivation, the soil Cd content of the plow layer increases from the background level 0.22 mg kg⁻¹ to 0.40 mg kg⁻¹. The accumulation of Cd in the plow layer is in proportion to the external inputs and is affected by the soil and plant characteristics, and management practices. The model can be used to evaluate the environmental fates of other toxic element in soils with case specific parameters.     

Geochemical background values for trace elements in arable soils developed from sedimentary rocks of glacial origin

The total content of trace elements was examined in some arable soils developed from boulder loam and silt formations of the Middle Poland and Baltic glaciations (62 profiles). Mean element concentrations calculated on the basis of chemical and statistical analyses were as follows: Mn = 322; Zn = 36; Cr = 30; Ni = 12.7; Pb = 10.3; Cu = 8.8; Co = 4.7; and Cd = 0.27 in mg kg^–1 of soil dry weight. The authors propose to accept these figures as the geochemical background values for soils derived from sedimentary rocks of glacial origin.     

Urban geochemistry: A study of element distributions in the soils of tallinn (Estonia)

First results are presented from the Urban geochemistry of Tallinn, a project supported by the Scientific and Environmental Affairs Division of NATO. The distribution of chemical elements in 532 samples of the topsoils from the territory of the biggest industrial centre of Estonia (pop. 500,000) is interpreted. Statistical analysis and mapping of major and trace elements at the territory of the Tallinn region and of the city were performed and background values and local anomalies of chemical elements on the territory were determined. The investigation focussed on the determination of zones with anomalously high concentrations of elements and the relationships of soil contamination with different pollution sources. The increase of the element concentrations has natural as well as anthropogenic origins. A detailed comparative analysis of the element distributions and the results of a factor analysis showed that the distribution of the major chemical elements depended mainly on the composition of the underlying sedimentary rocks.The territory of Tallinn is characterised by relatively high and widespread concentrations of Ba, Cr, Ga, Ni, Ti and Zn. Especially intensive local concentrations were determined for As, Cr, Mn, Ni, Pb, S, V and Zn, which are typical for the local pollution of the soils by industrial sources. The levels of As, Cr, Mn and V are more than three times. Pb and Zn are more than five times higher in the geochemical anomalies than for background levels. For the Tallinn region two major associations of elements connected with industrial pollutions of the soil are typical: the first association includes Ba, Cr, Mn, Ni and partly Fe and the second one includes As, Pb and Zn. For the city of Tallinn an increase of Ag, Ba, Be, La, Pb, Sn and Zn concentration in the soil was detected. Ba, Cr, Mn and Ni occur in high concentrations in the soils around Maardu. Different types of contamination sources can be identified in Tallinn and its suburbs.     

Konzentrationen von Schwermetallen in Bodenlösungen aus bayerischen Wäldern

Goal and Methods

During two years, soil solution samples were collected at 18 forest sites with low anthropogenic heavy metal loads in Bavaria using ceramic suction cups. The collected samples were analysed for pH, conductivity, dissolved organic compounds, and the trace elements Al, Cr, Fe, Mn, Ni, Cu, Zn, Cd, Ba, and Pb.

Results

In addition to initial interference effects caused by the installation of suctions cups, time series were characterised by seasonal variations. The results obtained for the replicated suction cups were comparable for every individual area with standard deviations of 20 to 25 percent. With increasing soil depth, the pH of the soil solution increases specifically at those sites (up to 2.5 pH units) where the topsoils have been acidified. On the other hand, concentrations of all trace elements investigated — excepted of Al and Mn — are not influenced by the soil depth. The forest stand has no significant additional effect on trace element concentrations. Contents of Al, Mn, and Zn are correlated with low pH-values in the soil solution, whereas the mobilisation of Ba is mainly caused by ion exchange. Complexes of trace elements and dissolved organic matter were only detected for Cu at one site. Element concentrations in the soil solution are not significantly influenced by the contents of aqua regia soluble portions in the soil matter. Only very high qua soluble portions increase the concentrations in the soil solution. The overall heavy metal concentrations determined in soil solutions are low compared with different limiting and threshold values, respectively.

Conclusions

Trace element concentrations in soil solutions are mainly influenced by the soil properties themselves. The contribution of the forest stand is negligible. Therefore, from the ecotoxicologic point of view, the risk of leaching heavy metals contaminating the groundwater is not significant for the investigated forest sites and without any respect to silviculture practices.     

福建丰产荔枝园土壤微量元素含量的研究

与我国红壤平均水平相比，福建丰产荔枝园土壤有效态锌、钼及水溶态硼含量较高，而活性锰及有效铜含量较低；土壤全锌、锰、钢量亦较低。在土壤ｐＨ４．５４—８．７６时，ｐＨ值与有效态钼含量呈较显著正相关，而与代换态锰、水溶态硼、有效态铁含量呈显著或极显著负相关。本文初步提出福建荔枝园土壤微量元素含量的适宜指标，可供土壤营养诊断及平衡施肥之参考。     

三江平原泥炭地微量元素垂直分布特征

采用冬季采样，现场分层的方法，系统地研究了三江平原河床-河漫滩型泥炭地和谷底洼地型泥炭地微量营养元素和有益元素的垂直分布特征。结果表明，微量营养元素Cu、Zn、Fe、Mn、B和有益元素Ni、Sr、Ti、V、Co均有在G层急剧积累的趋势，Fe、Mn、B、Zn、Ti、Sr质量分数在Ase层明显高于泥炭层，某些微量元素间具有显著的相关性。