热脱附-气相色谱法测定环境空气中芳烃和卤代烃

建立了热脱附-气相色谱法测定环境空气中9种芳烃和卤代烃方法。阐述了样品管制备、采样袋预处理、现场采样和实验富集等过程。采用保留时间定性、外标法定量。进行了自动热脱附仪的吸附和解吸效率的试验,各组分的吸附效率均在97%以上,解吸效率达98 9%。最低检出质量浓度氯乙烯为0 0003mg/m3、1,2-二氯乙烷和1,2-二氯丙烷为0 0002mg/m3、苯、甲苯、乙苯、对二甲苯、苯乙烯和邻二甲苯均为0 0001mg/m3。试图以不更换TenaxTA吸附剂标准冷阱来测定齐鲁石化环境空气中特征污染物乙烯,由于冷阱对乙烯的二级吸附未能很好地解决,试验效果不理想,有待进一步研究。     

固相微萃取-气相色谱-质谱法测定水中痕量有机磷和阿特拉津农药

采用PA萃取纤维吸附水中敌敌畏、乐果、内吸磷、甲基对硫磷、对硫磷、马拉硫磷等6种有机磷和阿特拉津农药,在气相色谱-质谱仪进样口热解吸后进行检测.筛选比较了几种萃取纤维,优化了萃取方式、萃取时间、离子强度、pH、解吸温度和解吸时间等萃取条件.方法适用于多类型水体中6种有机磷和阿特拉津农药的分析.     

PAN-S树脂富集钴的分光光度法测定研究

研究了PAN—S浸渍树脂对Co^2＋的吸附性能。Co^2＋吸附pH值范围为4．7—9．2，最佳pH值为5．4；达到最大吸附容量需25min，树脂对Co^2＋平衡吸附容量是98mg／g干树脂，达到最大吸附容量平衡时用0．1mol／L的HNO，洗脱，洗脱率达98％。该方法建立了PAN—S-树脂富集一分离钴离子的分光光度测定方法，结果令人满意。     

金膜吸附-冷原子吸收光谱法测定空气中的汞

采用新型金膜吸附-冷原子吸收光谱法测定空气中的汞，在0μg/L～100μg/L范围内线性良好，相关系数为0．9991。方法检出限为1．6 ng/m3，RSD为0．5％～2．7％，测定两种不同浓度的汞标准样品，相对误差为6．1％和3．2％。与两种现行国标方法（巯基棉富集和高锰酸钾溶液吸附法）比较，该方法所需试剂种类少，操作简便、吸附效率好，加标回收率高。     

固定源硫酸雾国内外采样方法优劣分析

固定污染源硫酸雾的国标采样方法为滤筒法，但对其采样效率研究较少。在调研国内外标准方法及相关文献的基础上，通过大量实样测定，对国标采样法进行改进：在内装滤筒的烟尘采样管后串联一个冲击式吸收瓶，此改进方法弥补了国标漏测气态硫酸雾的缺陷，采样效率达到99％以上，国标法仅为改进法的47％～68％。将国标改进法与USEPA采样法进行比对，结果表明，由于中国环境本底颗粒物浓度较高，硫酸雾易吸附于颗粒物上，致使USEPA采样效率仅为国标改进法的2?4％～12％。     

废气净化装置排气中有机污染物的气相色谱/质谱分析

利用活性炭对有机污染物具有较强的吸附和定量解吸的能力，对废气净化装置排气中的有机污染物进行吸附采样、溶剂解吸及气相色谱／质谱分析，可以克服气相色谱法依赖标样保留值定性的不足，扩大了定性范围，提高了准确度。     

硅胶管吸附气相色谱法测定气体中的乙酸、丙酸

建立了用GC-FID同时测定空气中乙酸、丙酸的方法.乙酸、丙酸经硅胶管吸附后,用丙酮溶剂解吸,气相色谱分析.优化条件下,在20 ～2 000 mg/L范围内有良好的线性关系.方法检出限分别达到了1.0 mg/m3和0.5 mg/m3,相对标准偏差2.2％和1.9％,回收率在94％以上.     

钼磷酸氧化萜烯醇光度法测定矿山废水中松脂油（二号油）

在文献的基础上，利用钼磷酸在浓硫酸作用下于乙醇介质中优先氧化萜烯酸及其衍生物，而本身被还原为钼兰的性质，本文建立了测定矿山废水中松脂油的方法，方法检出限为０．００６ｍｇ／５ｍｌ，回收率在８８％—１０７％之间，相对标准偏差为５．０５％。本文还对钼磷酸的溶剂选择，钼磷酸和浓硫酸的用量对吸光度的影响，以及浓盐酸的用量对萃取效率影响做了详细研究。     

微波技术在环境试样处理中的应用

综述了微波技术在样品消解、干燥以及溶剂萃取和解吸、生色反应、形态分析、微波雾化等方面的应用。比较了微波技术优于传统预处理技术之处。经分析认为该技术具有广阔的推广和应用前景。     

毛细管低温吸附气相色谱法同时测定空气中痕量甲硫醇和硫化氢

建立了毛细管低温吸附气相色谱同时测定空气中痕量甲硫醇和硫化氢的方法，介绍了冷冻吸附装置的制备方法和样品冷凝吸附流程。甲硫醇和硫化氢分别在0.467ng～5.16ng和0.327ng～3.60ng范围内线性良好，当进样体积为1L时，检出限为0．205μg/m^3和0．213μg／m^3，空白加标平均回收率为88．6％和90．2％，RSD为6.0％和6．5％。     

Multiple kinetic Langmuir modeling to predict the environmental behaviour of As(v) in soils

A soil with a relatively high Fe content (2.82% [w/w]) was loaded for up to one year with As(v) by equilibrating it with a solution containing 1000 mg l(-1) As(v) at a soil mass-to-solution ratio of 0.1 kg l(-1). The incorporation of As(v) into the soil and its distribution over the soil phases were monitored by sampling at strategic time intervals using an operationally defined five-step sequential extraction procedure (Wenzel et al., Anal. Chim. Acta, 2001, 436, 309) and subsequent As measurement. A multiple kinetic Langmuir model was developed to retrieve the dynamic parameters (adsorption and desorption rate constants, capacities and Langmuir equilibrium constants) for each of the soil phases by numerical fitting of the experimental adsorption data to the model. Under the equilibration conditions used the adsorption rate constants for all five operationally defined soil phases were very similar but the desorption rate constants decreased by a factor of ca. 150 from soil phase 1 (non-specifically sorbed As) to 5 (residual phases). This implies that As(v) incorporation "deeper" into the soil leads to stronger binding which is associated with the Langmuir equilibrium constants (adsorption rate constants/desorption rate constants). Equilibration of the soil with As(v) was complete in ca. 10 days with As(v) predominantly bound to soil phase 2 (specifically sorbed As) and soil phase 3 (amorphous and poorly crystalline hydrous oxides). X-Ray absorption spectroscopy techniques revealed that these binding characteristics may be related to adsorption of As(v) on Si- and/or Al-containing structures and natural hydrous iron oxide (HFO) surface sites, respectively. Since the model is independent of the initial As(v) concentration in the solution and the soil mass-to-solution ratio, the behaviour of the thus characterized soil-As(v) system can be predicted for a range of conditions. Simulations showed that in an accidental As(v) spill the soil studied would actively scavenge As(v) by instantaneous adsorption onto all soil phases followed by redistribution of As(v) from weaker binding sites to stronger ones over time.     

Soil-Water Partitioning and Desorption Hysteresis of Volatile Organic Compounds from a Louisiana Superfund Site Soil

The adsorption and desorption of three volatile organic compounds (1,2- dichloroethane, 1,1,2- trichloroethane and 1,1,2,2-tetrachloroethane) from a previously uncontaminated clayey soil sample from a Superfund site in North Baton Rouge,Louisiana was studied. In the linear range of the adsorption isotherm, the partition constants were not affected by the presence of the co-solutes. The adsorption isotherms over a wide concentration range on the soil followed the nonlinearFreundlich isotherm. The desorption of the compounds showedsignificant hysteresis at all concentrations studied. Approximately 20 to 70% of the adsorbed mass of organic compounds resisted the desorption even after five months ofsuccessive desorption steps. The desorption of four compounds(1,2-dichloroethane, 1,1,2-trichloroethane, 1,4-dichlorobenzeneand hexachlorobutadiene) from a contaminated soil sample fromthe same site was also studied. The aqueous concentration declined as the successive desorption steps progressed. For hexachlorobutediene the desorption can be visualized as occurring in two stages. The first stage involved a loosely bound or reversible fraction and the second stage involveda tightly bound or resistant fraction.     

环境空气中丙烯酸乙酯的气相色谱法测定

建立了环境空气中丙烯酸乙酯的TenaxGC吸附 -热解吸气相色谱测定方法。方法回收率为 87 3%～1 0 7 1 % ,变异系数为 5 3%～ 7 2 %。当采样体积为 2L时 ,检测限为 0 0 2mg/m3,具有采样时间短 ,不用任何溶剂等特点。     

土壤中铁氧化物对铅吸附-解吸的影响

选择上海地区广泛分布的水稻土,通过静态吸附平衡试验,比较土壤去除非晶质氧化铁和去除游离氧化铁后对Pb2+的吸附-解吸行为,采用数学模型拟合,探讨3种土壤的最佳拟合方程、最大吸附的理论值和亲和能力,进而研究非晶质氧化铁和游离氧化铁对Pb2+吸附-解吸的影响。结果表明,去除氧化铁后吸附能力和亲和能力均减弱,原土的最大吸附量为29.21 g/kg,非晶质氧化铁的贡献值为3.52 g/kg,游离氧化铁的贡献值为8.32 g/kg。     

Adsorption and leaching of novel fungicide pyraoxystrobin on soils by <Superscript>14</Superscript>C tracing method

Pyraoxystrobin, (E)-2-(2-((3-(4-chlorophenyl)-1-methyl-1H-pyrazole-5-yloxy)methyl)phenyl)-3-methoxyacrylate, is a newly developed strobilurin fungicide with high antifungal efficiency. It has high potential to enter soil environments that might subsequently impact surface and groundwater. Therefore, ¹⁴C-labeled pyraoxystrobin was used as a tracer to study the adsorption/desorption and migration behavior of this compound under laboratory conditions in three typical agricultural soils. The adsorption isotherms conformed with the Freundlich equation. Single factor analysis showed that organic matter content was the most important factor influencing the adsorption. The highest adsorption level was measured in soil with low pH and high organic carbon content. Once adsorbed, only 2.54 to 6.41% of the adsorbed compound could be desorbed. In addition, the mobility results from thin-layer chromatography and column leaching studies showed that it might be safe to use pyraoxystrobin as a fungicide without causing groundwater pollution from both runoff and leaching, which might be attributed to its strong hydrophobicity. High organic matter content enhanced pyraoxystrobin adsorption and desorption because of the rule of similarity (lipid solubility). In the column leaching study, 95.02% (minimum value) of the applied ¹⁴C remained within the upper 4.0-cm layer after 60 days.     

改性泥炭对重金属离子的吸附

为了研究泥炭对重金属离子（Pb^2＋、Cu^2＋、Cd^2＋、Cr^6＋、Ni^2＋）吸附率的各种影响因素，依次进行了溶液pH、振荡时间、改性泥炭投加量、溶液初始浓度等条件试验。结果表明，改性后的泥炭在最适合的条件下，对这5种金属离子都有较强的去除效果，5种金属离子的最大吸附效率均在9096以上。     

Estimation of phosphorus flux in rivers during flooding

Reservoirs in Taiwan are inundated with nutrients that result in algal growth, and thus also reservoir eutrophication. Controlling the phosphorus load has always been the most crucial issue for maintaining reservoir water quality. Numerous agricultural activities, especially the production of tea in riparian areas, are conducted in watersheds in Taiwan. Nutrients from such activities, including phosphorus, are typically flushed into rivers during flooding, when over 90 % of the yearly total amount of phosphorous enters reservoirs. Excessive or enhanced soil erosion from rainstorms can dramatically increase the river sediment load and the amount of particulate phosphorus flushed into rivers. When flow rates are high, particulate phosphorus is the dominant form of phosphorus, but sediment and discharge measurements are difficult during flooding, which makes estimating phosphorus flux in rivers difficult. This study determines total amounts of phosphorus transport by measuring flood discharge and phosphorous levels during flooding. Changes in particulate phosphorus, dissolved phosphorus, and their adsorption behavior during a 24-h period are analyzed owing to the fact that the time for particulate phosphorus adsorption and desorption approaching equilibrium is about 16 h. Erosion of the reservoir watershed was caused by adsorption and desorption of suspended solids in the river, a process which can be summarily described using the Lagmuir isotherm. A method for estimating the phosphorus flux in the Daiyujay Creek during Typhoon Bilis in 2006 is presented in this study. Both sediment and phosphorus are affected by the drastic discharge during flooding. Water quality data were collected during two flood events, flood in June 9, 2006 and Typhoon Bilis, to show the concentrations of suspended solids and total phosphorus during floods are much higher than normal stages. Therefore, the drastic changes of total phosphorus, particulate phosphorus, and dissolved phosphorus in rivers during flooding should be monitored to evaluate the loading of phosphorus more precisely. The results show that monitoring and controlling phosphorus transport during flooding can help prevent the eutrophication of a reservoir.     

Retention capacities of several bryophytes for Hg(II) with special reference to the elevation and morphology of moss growth

Hg(II) Retention capacities of nine bryophyte species, collected from Jinfo Mountains (JFM) in Chongqing, China, had been investigated with special reference to the effect of morphology and elevation of moss growth. Results indicated that adsorption capacities of bryophytes for Hg(II) became stronger with the increase of multi-branches and leafy-shoots, as well as the elevation of moss growth, which was observed both in adsorption isotherm and adsorption kinetics experiments. Contrarily, the desorption kinetics showed a decrease tendency with the increase of multi-branches and leafy-shoots and the elevation of moss growth. The results demonstrated that bryophytes with higher multi-branches and leafy-shoots and higher growth elevation had a stronger adsorption capacity and a weaker desorption tendency, and therefore had a stronger retention capacity to Hg(II). The results disclosed the different relative sensitivity and retention capacity of mosses to pollution resulting from heavy metals, due to the differences in growth elevation and morphology. These should be considered when bryophytes were chosen as a tool for biomonitoring materials to environmental pollution, especially caused by Hg(II).     

Recovery of sulfate saturated soils in the Plynlimon catchments, mid-Wales following reductions in atmospheric S inputs from the 1980s to 2011

Sulfate adsorption capacity of B-horizons of base-poor, predominantly stagnopodzol, soils from the Plynlimon catchments, mid-Wales was determined by combination of laboratory adsorption and desorption isotherms. Results show that sulfate adsorption capacity of a range of stagnopodzol (Histic-stagno-podzol (Leptic), WRB), brown podzolic soil (Histic-umbrisol (Leptic), WRB) and stagnohumic gley (Histic-stagno-gleysol, WRB) B-horizons was positively related to the amounts of extractable (pyrophosphate and oxalate) Fe + Al, with the stagnopodzol and brown podzolic soil Bs horizon having the largest adsorption capacity and stagnohumic gley Bg horizon the smallest adsorption capacity. Results show that dissolved organic carbon (DOC) has a negative but limited effect on sulfate adsorption in these soils. Results obtained from a set of historical soil samples revealed that the grassland brown podzolic soil Bs horizon and afforested stagnopodzol Bs horizon were highly saturated with sulfate in the 1980s, at 63% and 89% respectively, whereas data from some recently sampled soil from two sites revisited in 2010-11 indicates that percentage sulfate adsorption saturation has since fallen substantially, to 41% and 50% respectively. Between 1984 and 2009 the annual rainfall-weighted mean excess SO(4)-S concentration in bulk precipitation declined linearly from 0.37 mg S l(-1) to 0.17 mg S l(-1). Over the same period, flow weighted annual mean stream water SO(4)-S concentrations decreased approximately linearly from 1.47 mg S l(-1) to 0.97 mg S l(-1) in the plantation afforested Hafren catchment compared to a drop from 1.25 to 0.69 mg S l(-1) in the adjacent moorland catchment of the Afon Gwy. In flux terms, the mean decrease in annual stream water SO(4)-S flux has been approximately 0.4 kg S ha(-1) yr(-1), whilst the recovery in stream water quality in the Afon Cyff grassland catchment has been partly offset by loss of SO(4)-S by desorption from the soil sulfur pool of approximately 0.2 kg S ha(-1) yr(-1).