矿区周围土壤中重金属危害性评估研究

分别用总量法和连续萃取法对广东大宝山矿周围土壤、植物和沉积物中重金属的总量和化学形态进行了详细分析。结果发现，矿山废水流入的横石河沉积物中Pb、Zn、Cu和Cd的质量分数分别为1841．02、2326．28、1522．61和10.33mg／kg；经此河水灌溉的稻田中重金属(Cu、Cd、Pb和Zn)的质量分数也远远超出了土壤环境二级标准值，其中Cu、Cd超标倍数分别为14．01和4．17倍。结果还表明，生长在矿区周围的植物也受到不同程度重金属的污染且不同植物吸收和积累重金属的能力相差很大。用Tessier连续法对土壤中重金属进行萃取发现，虽然重金属主要存在于残余态中，但在Fe-Mn氧化态、有机结合态中的质量分数也很高．说明这些土壤确实受到了有毒有害重金属元素的严重污染。     

添加羟基磷灰石对土壤铅吸附与解吸特性的影响

采用羟基磷灰石对四种不同类型的土壤进行铅的吸附-解吸试验.结果表明:四种土壤对铅的吸附均可用Langmuir和Freundlich方程进行描述,土壤中加入羟基磷灰石明显增加了土壤对铅的吸附量和吸附亲和力,同时降低了土壤中铅的解吸百分数,在偏酸性的红壤上表现更为明显,其最大吸附量增加28%.羟基磷灰石对铅吸附的反应机理可能与磷灰石溶解后与铅形成磷酸盐沉淀及其对铅的表面吸附作用有关.土壤对铅的吸附量及吸附亲和力与土壤的有机质、阳离子交换量及粘粒含量有显著正相关,而与土壤砂粒的含量呈负相关.     

Distribution of heavy metal contents of urban soils in parks of Seville

Several metals in urban soils of Seville were extracted by two methods, which respectively give estimates of the available and ‘quasi total’ contents. Although the soils did not show strong heterogeneity in their general properties, high dispersion of the contents in those metals with greater relative availability, Cu, Pb and Zn, as compared to others suggested that pollution with these three metals could occur in some sampling sites. It was shown that the contents in these metals tend to increase as the historic quarters of the city are approached. Using reference values given by the Québec Ministry of Environment it was shown that those green areas closer to the historic centre present contents in Pb, Zn and particularly Cu that often exceed the acceptable limits for residential, recreational and institutional sites. From background contents for Seville soils estimated from a park located on the outskirts, a pollution load index (PLI) for each sampling site was calculated for the set of these three metals. It was shown that the PLI tends to increase as traffic density increases and as distance from main traffic decreases, but poor regressions were obtained, suggesting that other variables different from traffic should be considered.     

Response of Lupinus albus to Pb–EDTA indicates relatively high tolerance

White lupin plants were grown in hydroponics with 0, 90 and 180 µmol L^?1 Pb(II) ethylenediaminetetraacetate complex for 30 days. Pb distribution (shoot/root ratio) was 0.34 and 0.46 for both Pb treatments. In the shoots, no decrease in biomass nor in photosynthetic pigment levels and no changes in the concentrations of malondialdehyde and glutathione were detected. In the roots, malondialdehyde increased by 20%, glutathione 2–3.6 times and phytochelatin concentrations 4–5 times. The high tolerance of white lupin makes it a valuable plant for phytoremediation of Pb-contaminated soil.     

Biogeochemical reductive release of soil embedded arsenate around a crater area (Guandu) in northern Taiwan using X-ray absorption near-edge spectroscopy

This study investigates biogeochemical reductive release of arsenate from beudantite into solution in a crater area in northern Taiwan,using a combination of X-ray absorption near-edge structure (XANES) and atomic absorption spectrometry.Total arsenic (As) concentrations in the soil were more than 200 mg/kg.Over four months of laboratory experiments,less than 0.8% As was released into solution after reduction experiments.The 71% to 83% As was chemically reduced into arsenite (As(III)) and partially weathering into the soluble phase.The kinetic dissolution and re-precipitation of As,Fe,Pb and sulfate in this area of paddy soils merits further study.     

UPLC法同时快速测定湿地土壤中的五种低分子量有机酸

研究了超高效液相色谱（UPLC）法同时测定湿地土壤中柠檬酸、草酸、苹果酸、酒石酸和丁二酸等5种有机酸的方法,并测定了武昌湖、巢湖和鄱阳湖湿地土壤样品中的有机酸组成含量,为揭示有机酸在土壤-植物-根际环境中的转运、分配和分泌提供理论依据。结果表明：利用UPLC法可以快速地分离5种有机酸,比HPLC分离时间缩短1倍左右;各有机酸的加标回收率为99.17%～103.55%,相对标准偏差为0.48%～1.92%,检测限为0.05～0.18 mg/kg,该方法线性关系优良（R²>0.997）;除了鄱阳湖湿地土壤样品的酒石酸未能检测出,其他湿地土壤样品中的5种有机酸都能检测出;不同湿地土壤样品的优势有机酸种类不同,武昌湖湿地土壤中的柠檬酸和苹果酸对有机酸总量贡献较大,巢湖湿地土壤中的柠檬酸对有机酸总量的贡献最大,鄱阳湖湿地土壤中丁二酸占有机酸总量的比例小于10%;湿地土壤有机酸含量多集中在土壤深度为30～50 cm处,这与该区域植物根系分布及微生物活性较高有关。     

Adsorption–desorption behavior of atrazine on agricultural soils in China

Adsorptionanddesorptionareimportantprocessesthataffectatrazinetransport,transformation,andbioavailabilityinsoils.Inthisstudy,theadsorption–desorptioncharacteristicsofatrazinein three soils (laterite, paddy soil and alluvial soil) were evaluated using the batch equilibrium method. The results showed that the kinetics of atrazine in soils was completed in two steps: a “fast” adsorption and a “slow” adsorption and could be well described by pseudo-second-order model.In addition,the adsorption equilibrium isotherms were nonlinear and were well fitted by Freundlich and Langmuir models. It was found that the adsorption data on laterite, and paddy soil were better fitted by the Freundlich model;as for alluvial soil,the Langmuir model described it better. The maximum atrazine sorption capacities ranked as follows: paddy soil > alluvial soil > laterite. Results of thermodynamic calculations indicated that atrazine adsorption on three tested soils was spontaneous and endothermic. The desorption data showed that negative hysteresis occurred. Furthermore, lower solution pH value was conducive to the adsorptionofatrazineinsoils.Theatrazineadsorptioninthesethreetestedsoilswascontrolled by physical adsorption, including partition and surface adsorption. At lower equilibrium concentration, the atrazine adsorption process in soils was dominated by surface adsorption;while with the increase of equilibrium concentration, partition was predominant.     

三峡澎溪河流域消落区与岸边土壤磷形态特征

选取了落干期澎溪河流域6个消落区点位,分析了消落区土壤磷形态分布特征,并探讨了各形态磷之间的相关性.结果表明,(1)采用SMT法测定了消落区土壤总磷、无机磷和有机磷含量,其总磷TP含量均值为575.29 mg·kg~(-1),有机磷OP含量均值为91.23 mg·kg~(-1).(2)采用Hedley法分析了消落区土壤磷的5种赋存形态,其中WA-Pi、PA-Pi、Fe/Al-Pi等3种易迁移的无机磷形态之和占可提取Pi的11.61%,且低于岸边土壤;WA-Po、PA-Po两种生物可利用性较高的有机磷形态含量之和占可提取Po的22.28%,而中活性有机磷Fe/Al-Po占可提取Po的66.30%,且消落区土壤各形态Po含量均低于岸边土壤,又以Fe/Al-Po含量差异最大.(3)消落区土壤TP与活性较强的WA-Pt、PA-Pt呈显著相关,表明消落区土壤活性磷含量主要受TP影响;各形态磷之间不具有显著相关性,表明不同形态磷的来源可能不同;消落区土壤Fe/Al-Pt与土壤有机质OM呈显著相关,表明土壤有机质的含量可能影响铁铝结合态磷含量.在淹水条件下,消落区土壤磷组分的释放对上覆水体的潜在影响不容忽视.     

影响土壤中钴活性的因素

用大样本统计分析上土壤性质对钴活性的影响及研究改变土壤ｐＨ值，有机质和氧化还原状况对钴活性的影响。结果表明，在其它土壤性质不变情况下，全钴提高，活性钴的数量增加，锰氧化物的作用则相反，在酸性及还原土壤中，土壤ｐＨ值，浸提剂ｐＨ值对钴的提取量有极显的影响；在中性和碱性并处于氧化状态的土壤中，影响不显，增加土壤有机质可以提高活性钴的数量。     

悬浮液进样FAAS法测定黄棕壤中的微量铜

本文采用悬浮进样火焰原子吸收光谱法测定黄棕壤中微量铜 ,并对样品的研磨时间、悬浮液浓度、酸度选择及校正方法等进行了探讨。实验表明 :该法的检出限 (K =3)为 0 .12μg· g-1,精密度 (RSD)为4.6 % ,加标回收率为 98～ 10 6 % ,对水系沉积物 GSD5、GSD6标准样品测定结果与推荐值吻合。