红树林湿地土壤矿物的分析

以湛江湾南海堤典型红树林湿地土壤为研究对象,采用X射线衍射(XRD)和傅立叶变换红外光谱(FTIR)快速批量鉴定土壤中矿物成分,利用扫描电子显微镜(SEM)观察土壤颗粒形貌特征并获得化学成分组成信息;同时采集附近光滩土壤样品进行对比研究,以揭示红树林湿地土壤特殊的生态环境特征。结果表明,红树林湿地土壤矿物主要由高岭石、石英、白云母、埃洛石、地开石和蛇纹石等组成;与光滩土壤相比,红树林湿地土壤矿物类型多样,而光滩土壤矿物相对单一,主要为石英和高岭石;红树林湿地土壤颗粒以片状聚合体为主,主要元素组成为C、O、S、Al、Si、Mg、Fe等,常见含有Cu、Zn、Mo等重金属元素。同时发现红树林湿地土壤颗粒含有较丰富的硫化物;而光滩土壤未发现上述特征,表明红树林湿地处于一个特殊的生态环境,土壤沉积物中富含有机质、Fe、S等,比一般潮滩更易于富集硫化物或重金属。     

菜园土壤中的铜及其与土壤有机碳的关系

通过野外调查与室内分析相结合的方法研究了杭州市郊主要菜园土壤中铜的状况,并对其与土壤有机碳的关系作了探讨.取样分析结果表明,调查区域菜园土壤全铜含量在4.3×10-6～205.5×10-6之间,平均为(43.6±36.7)×10-6,有效铜含量在0.17×10-6～6.18×10-6之间,平均为(2.70±1.46)×10-6.同时还发现,菜园土壤有效铜含量与全铜含量呈极显著正相关,相关系数为0.717**(n=45,P=0.01,下同),据此认为菜园土壤有效铜的供给是以全铜量为基础的.相关分析还得出,全铜含量与总有机碳和易氧化碳含量均呈极显著正相关,相关系数分别为0.695**和0.594**;有效铜含量也与总有机碳和易化有机碳含量呈极显著正相关,相关系数分别为0.666**和0.557**,这表明施用有机肥料可能是菜园土壤铜营养的重要来源之一.另外,菜园土壤铜的有效性也有随土壤总有机碳和易氧化有机碳含量的提高而增大的趋势,这对一般情况下提高土壤的供铜强度是有益的.但是,倘若土壤中已积累了过量的铜,则有可能加剧铜的毒害,蔬菜生产和菜园土壤管理中都应予以足够的重视.     

色谱法分析环境中铝形态的进展

综述了色谱法在环境体系铝形态研究中的应用进展,比较了离子交换色谱、体积排阻色谱、反相高效液相色谱、快速蛋白质液相色谱、毛细管电泳以及流路中嵌入色谱小柱的流动注射分析法的优缺点。引用文献55篇。     

A PRELIMINARY STUDY ON THE IMPACT OF MESOSCALE IRRIGATION OVER ARID LAND ON MESOSCALE CLIMATE

The present study investigated the modification of mesoscale inhomogeneous distribu-tion of soil wetness, resulting from mesoscale irrigation over arid or semiarid lands in mid-latitude in the later summer or early autumn, on mesoscale climate under conditions withand without synoptic flow influence, using an interactive model between soil and atmo-sphere. The simulations indicated that after a mesoscale irrgation, a wet soil breeze circu-lation was thermally forced, which was, in many features, similar to that of the sea breezecirculation. The influence of synoptic flows on the structure of thermally--induced wet soilbreeze circulation was also discussed.     

Semi-micro solvent extraction as a rapid and efficient preconcentration technique for the determination of n-alkanes in oil-contaiminated water and soil samples by capillary gas chromatography

Summary In this study, a rapid and efficient semi-micro extraction procedure is presented for the extraction of some higher n-alkanes from water and soil samples. In the case of water samples n-hexane was used as the organic phase in a phase volume ratio (volume of aqueous phase/volume of organic phase) higher than 285, while in the case of soil samples, extraction with n-hexane was carried out in the presence of an excess of 2 M NaCl solution. The extraction rate from soil samples is very high and is better than Soxhlet extraction, comparable with supercritical fluid extraction. High preconcentration factor in water samples allows the limits of detection to be in the ng.mL⁻¹ level with the use of gas chromatographic analysis. Flame ionization detector was used for monitoring the analytes. The obtained recoveries of all studied compounds from both water and soil samples are higher than 90%. This method was successfully used to determine some n-alkanes in municipal wastewater and contaminated soil.     

Arsenic Speciation in As(III)- and As(V)-Treated Soil Using XANES Spectroscopy

Arsenic (As) is a toxic trace element that occurs naturally in groundwater and soils. Understanding the reactions of arsenite (As(III)) and arsenate (As(V)) with soil and mineral surfaces is critical for predicting the fate and transport of As in the environment and developing better ways to remediate As-contaminated areas. This investigation uses X-ray absorption near edge spectroscopy (XANES) to evaluate the solid phase oxidation state and mineral surface binding sites in three agricultural soil samples from California, USA by fitting linear combinations of XANES spectra derived from several synthetic and well characterized As(III)- and As(V)-treated model compounds (Fe and Al metal hydroxides and aluminosilicate illite clay mineral). The results suggest that As(III) is either partially or completely oxidized to As(V) when reacted with soil in an aqueous, batch reaction. The As(III)-treated Aiken soil was composed of 60% As(III) attached to surfaces similar to lepidocrocite (γ-FeOOH)) and 40% As(V) attached to aluminosilicate (illite). The Fallbrook soil completely oxidized As(III) and the product was As(V) adsorbed on Al hydroxide (gibbsite, γ-Al(OH)₃) (62%), illite (16%), and lepidocrocite (γ-FeOOH) (22%). The reaction of As(III) with Wyo soil resulted in 42% As(III) adsorbed on surface similar to goethite and 58% As(V) adsorbed on lepidocrocite. Arsenic(V) adsorption on soil resulted in stable As(V) surface complexes that were well described by XANES spectra from As(V) adsorption complexes on gibbsite, illite, and lepidocrocite.     

土壤环境中的硒对人和动物健康的影响

硒是人和动物必需的微量元素之一。土壤中的硒含量过多或过低，人和 动物都会出现地方性疾病。土壤中硒的含量与土壤母质、地形、气候条件和土壤条件性质等有关，调节土壤性质可以改善作物的含硒量。防治硒缺额症和硒中毒症，每天必需摄入适量的硒，以100－200μg为宜，但人体对硒的需要量也与食物成分有关。     

添加有机肥和葡萄糖对铜毒害旱地红壤微生物生物量的影响

在预培红壤中加入定量的有机肥和葡萄糖及不同浓度的Cu,25℃培养14d，测定了土壤微生物生物量C（Cmic),N(Nmic)。结果表明，存在有机肥和葡萄糖时，土壤中Cmic和Nmic随着Cu浓度的增加而降低；Cmic/Nmic随着Cu浓度的增加而增大。施加有机肥和葡萄糖的土壤中，在所有Cu处理浓度下，土壤中Cmic和Nmic均比未加有机物质处理高，特别是有机肥处理中土壤Cmic和Nmic均比其它处理高得多，说明有机肥可明显减轻Cu对土壤微生物生物量的毒性，同时也说明有机肥可提供微生物N源。不含Cu时，加入有机肥和葡萄糖导致土壤中Cmic和Nmic增加，其中有机肥明显。     

还原气化-原子荧光光谱法快速测定绿色食品基地土壤中的砷与汞

应用还原气化-原子荧光光谱法，使待测元素与基体自动分离、富集，测定绿色食品基地土壤中的AS、HG。经对国家经土壤标准物质进行分析证明，该方法具有快速、准确、灵敏度高等优点，用于绿色食品基地的审评检测，结果令人满意。     

土壤微生物ATP、脱氢酶和尿素酶活性的ED50值评价外源镧的生物毒性

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