以MnSO 4 作催化剂快速测定水中COD

建立了酸性条件下,以MnSO4代替Ag2SO4作催化剂快速测定水中COD的方法.考察了K2Cr2O7用量、MnSO4用量、H2SO4浓度、消解温度、消解时间等因素的影响,确定了最佳试验条件和最佳测定范围.方法精密度和准确度均能满足测定要求,与重铬酸钾法作对比试验,测定结果基本一致.     

用正交试验确定游离性余氯最佳测定条件

在用DPD光度法测定水中余氯时，对水样的pH值、显色时间、显色剂用量和反应温度进行了研究，通过正交试验系统地分析了各因素影响测定结果准确性的程度，并获得最佳的反应条件，表明在该条件下测定水中余氯的准确性优于其他条件下测定的结果。     

影响紫外法测定总氮的因素研究

用紫外分光光度法测定水中总氮时由于受到试剂质量、消化温度、消化时间、环境等因素的影响,往往使空白吸光值偏高,标准曲线线性和结果重现性差,直接影响测定结果.本文通过对上述因素的研究,提出保证测定质量的条件,找到消除干扰的方法.     

碘量法测定地表水溶解氧的改进

测定地表水中溶解氧的方法通常采用碘量法。但在分析过程中发现,此法硫代硫酸钠溶液的标定、溶解氧的固定、析出碘、滴定中均存在费时费试剂。本文为提高工作效率,节约试剂,对原试剂加入量、静置时间、取溶液量进行了改进,作了某些条件实验,并对河水样溶解氧作了对比测定,结果令人满意。     

水样总氮测定空白值偏高的探讨

根据《水质总氮的测定碱性过硫酸钾消解紫外分光光度法》（GB11894—89）测定地表水中的总氮时，空白试验的吸光值常偏高。经对加热消解时间、试验用水水质、试剂添加顺序、储存时间等因素进行了试验，并对操作步骤影响吸光度空白值作了探讨。     

氰化钾标准中间液保存时间试验

在《水和废水监测分析方法》（第四版）异烟酸-吡唑啉酮光度法测定总氰化物中，需将10mg／L氰化钾标准中间液在临用前再稀释10倍，配成1．0mg／L标准使用液。该方法没有对氰化钾标准中间液保存时间作明确要求，为保证分析结果的准确性，也为提高工作效率，对氰化钾标准中间液在2℃-4℃时的保存时间作试验，测定结果见表1。     

高锰酸盐指数测定方法的研究

着重介绍了测定水中高锰酸盐指数的方法和影响测定结果准确性的因素，通过大量实验结果表明样品的酸度，氧化剂的浓度，试剂加入的顺序，溶液的温度及加热时间等对样品的测定均有影响，其中加热时间的长短是关键影响因素。     

取样量与烘干时间对总悬浮物测定结果的影响

就取样量和烘干时间两个因素的变化对总悬浮物测定结果的影响程度进行了探讨。结果表明 ,取样量是造成悬浮物测定结果准确与否的主要因素 ,而不同的烘干时间对测定结果的精密度不会造成明显的影响。随着取样量的逐步减少 (从 2 0 0 0 ml减至 50 ml) ,平行样的相对偏差则从 2 7%上升到 4 5 5%。为了使相对偏差≤ 1 5% ,取水量必须满足其中的总不可滤残渣达到 6 2 mg以上。     

丙酮法和热乙醇法测定浮游植物叶绿素a的方法比对

将丙酮法和热乙醇法用于测定浮游植物叶绿素a,分析水样中是否加入碳酸镁、水样体积、萃取时间、萃取剂、破碎方法、离心时间、水样存放时间和滤膜样品存放时间等8个因素对测定的影响,并确定最佳试验条件。结果表明:2种方法的测定值之间有较好的线性关系,相比丙酮法,热乙醇法更具优势。     

变色酸法测定空气中甲醇的改进

对变色酸光度法测定空气中甲醇的方法进行了改进，在比色波长，显色时间和试剂用量等方面均作了重新选定，使精密度和准确度都有所提高，与气相色谱法比较，分析结果一致。     

Water Conservation Versus Soil Salinity Control

This paper tackles the increasingly significant problem of irrigation-induced soil salinity within a groundwater management model. Irrigation can result not only in heavier salt concentrations but also in the removal of salt from the soil through return flows. Given these contradictory observations, we are interested in the effects on soil salt concentration if irrigation efficiency is improved. We develop a model of salt concentration patterns in both soil and groundwater. We introduce a negative externality to the production process by assuming that soil degradation due to higher soil salinity affects total factor productivity. Within this framework, we show that in the presence of this externality, increasing irrigation efficiency can lead to higher or lower soil salt concentration, depending on the social cost of transferring salt from one reservoir to another.     

Assessing the wildlife habitat value of New England salt marshes: I. Model and application

We developed an assessment model to quantify the wildlife habitat value of New England salt marshes based on marsh characteristics and the presence of habitat types that influence habitat use by terrestrial wildlife. Applying the model to 12 salt marshes located in Narragansett Bay, RI resulted in assessment scores that ranged over a factor of 1.5 from lowest to highest. Pre-classifying the results based on marsh size and morphology helped to compare assessment scores between marshes, and demonstrated that even the lower ranking marshes had substantial habitat value. Stepwise multiple regression analysis of assessment scores and model components demonstrated that salt marsh morphology, the degree of anthropogenic modification, and salt marsh vegetative heterogeneity were significant variables and accounted for 91.3% of the variability in component scores. Our results suggest that targeting these components for restoration may lead to improved assessment scores for our study marshes. We also examined the use of lower resolution remote sensing data in the assessment in order to minimize the time and effort required to complete the model. Scores obtained using smaller-scale, lower resolution data were significantly lower than those obtained using larger-scale, higher resolution data (df = 11; t = 2.2; p < 0.001). The difference was significantly positively correlated with the portion of the assessment score that could be attributed to trees, pools, and pannes and marsh size (r (2) =0.50, F = 4.6, p = 0.04), and could indicate a bias against smaller, more heterogeneous marshes. We conclude that potential differences need to be weighed against the time benefit of using this type of data, bearing in mind the marsh size and the goals of the assessment. Overall, our assessment can provide information to aid in prioritizing marshes for protection and restoration, identify marshes that may harbor significant biodiversity, or help monitor changes in habitat value over time.     

新疆图木舒克地区土壤盐渍化空间分布特征

土壤盐渍化已成为影响图木舒克地区农业生产与生态环境的重要因素。本文以0~150 cm深度范围内土壤和地下水为研究对象,利用实际野外调查与数据统计分析的方法,研究得出:①强盐渍化主要分布于距离河流与渠道较远的地下水浅埋深区域,在纵向上表层聚盐现象明显,盐渍土类型随着土壤层深度加大从亚氯-亚硫酸盐渍土变为亚硫酸盐渍土。②土壤易溶盐含量与地下水化学类型在平面分布上吻合程度较高、与潜水矿化度呈正的高度相关性、与潜水埋藏深度呈负的中度相关性、沿潜水径流方向各层土壤盐渍化减弱。③当地下水埋深较浅时,潜水通过毛细管将易溶盐带入土壤表层,形成表层土壤盐渍化;地下水埋藏较深时,易溶盐分会随着降水淋滤和灌溉冲洗不断降低,地表盐渍化减弱。中、轻度盐渍化区域应控制灌溉用水矿化度,重度盐渍化及盐土区域可在建立排水系统的基础上采用泡田洗盐法。     

Quantification of Water, Salt and Nutrient Exchange Processes at the Mouth of A mediterranean Coastal Lagoon

Vassova lagoon is a typical Mediterranean (small, shallow, micro-tidal, well-mixed) coastal lagoon, receiving limited seasonal freshwater inflows from direct precipitation and underground seepage. An intensive study was carried out in order to quantify the mechanisms responsible for the intra-tidal and residual transport of water, salt, nutrients and chlorophyll at the mouth of this lagoon and to assess the lagoon's flushing behavior. Results indicated that although the system is micro-tidal, tidal effects appeared to be the dominant factor for the longitudinal distribution of physical and chemical parameters, while the associated residual flow is also important and serves as a baseline measure of overall circulation. However, analysis of the net longitudinal currents and fluxes of water, salt and nutrients revealed the importance of non-tidal effects (wind effect and precipitation incidents) in the mean tidal transport. It is shown that the Eulerian residual currents transported water and its properties inwards under southern winds, while a seaward transport was induced during precipitation incidents and northern winds. The Stokes drift effect was found an order of magnitude lower than the Eulerian current, directed towards the lagoon, proving the partially-progressive nature of the tide. Nutrients and chlorophyll-α loads are exported from the lagoon to the open sea during the ebb phase of the autumn and winter tidal cycles, associated with the inflow of nutrient-rich freshwater, seeped through the surrounding drainage canal. The reverse transport occurs in spring and early summer, when nutrients enter the lagoon during the flood tidal phase, from the nutrient-rich upper layer of the stratified adjacent sea. Application of a tidal prism model shows that Vassova lagoon has a mean flushing time of 7.5 days, ranging between 4 to 18 days, affected inversely by the tidal oscillation.     

Chemical characterization of precipitation at a coastal site in Trombay, Mumbai, India

Precipitation is the best scavenger for the particulates and dissolved gaseous pollutants present in the atmosphere. The chemical composition of precipitation is dominated by a number of in-cloud and below-cloud scavenging processes. The present study is aimed at analyzing the chemical composition of rainwater in the relatively less industrialized part of Mumbai. The pH of rainwater in this region ranges from 4.8 to 6.4. The percentage contributions of ions were calculated and the major contributing ions were calcium (28%), chloride (23%), sodium (18%), sulfate (14%), magnesium (11%), ammonium (4%), potassium (1%), and nitrate (1%). The correlation coefficient is highest for Na and Cl (r ²?=?0.99), giving a clear indication of contribution from sea salt. Sulfate and nitrate ions also show a very good correlation (r ²?=?0.90), which may be due to their coemission from fossil fuel combustion. Acidification caused by these ions is neutralized by Ca, Mg, and NH₄ ions. The neutralization effect due to these ions is validated by calculating the neutralization factor (NF). The NF values are in the order Ca > Mg > NH₄. The major source contributors for the ions in precipitation are sea salt (Na, Cl, and K) and fossil fuel combustion (SO₄ and NO₃). These assumptions are supported by the values of wet-only ratio, enrichment factor, and percent sea salt fraction.     

液相微萃取技术及其在环境水样预处理中的应用

介绍了液相微萃取技术的基本原理、萃取过程与中空纤维的形式。分析了中空纤维、有机萃取剂、吸收液体积、样品搅动、无机盐类、pH值和萃取时间等因素对萃取效果的影响。综述了液相微萃取技术在环境水样预处理中的应用。     

Remote-sensing-based analysis of landscape change in the desiccated seabed of the Aral Sea—a potential tool for assessing the hazard degree of dust and salt storms

With the recession of the Aral Sea in Central Asia, once the world’s fourth largest lake, a huge new saline desert emerged which is nowadays called the Aralkum. Saline soils in the Aralkum are a major source for dust and salt storms in the region. The aim of this study was to analyze the spatio-temporal land cover change dynamics in the Aralkum and discuss potential implications for the recent and future dust and salt storm activity in the region. MODIS satellite time series were classified from 2000–2008 and change of land cover was quantified. The Aral Sea desiccation accelerated between 2004 and 2008. The area of sandy surfaces and salt soils, which bear the greatest dust and salt storm generation potential increased by more than 36 %. In parts of the Aralkum desalinization of soils was found to take place within 4–8 years. The implication of the ongoing regression of the Aral Sea is that the expansion of saline surfaces will continue. Knowing the spatio-temporal dynamics of both the location and the surface characteristics of the source areas for dust and salt storms allows drawing conclusions about the potential hazard degree of the dust load. The remote-sensing-based land cover assessment presented in this study could be coupled with existing knowledge on the location of source areas for an early estimation of trends in shifting dust composition. Opportunities, limits, and requirements of satellite-based land cover classification and change detection in the Aralkum are discussed.     

Saltwater intrusion in coastal aquifer ??? comparison between the CIP and MOC simulation technique

Proper management and evaluation of environmental effects for coastal groundwater aquifers require accurate estimation of salt and fresh water movement. For this we compare two numerical methods to study saltwater intrusion. The two numerical methods are the CIP (constrained interpolation profile) and the MOC (method of characteristics). The two numerical methods are used to solve the salt transport equation. The two methods are applied and compared to saltwater intrusion experiments for confined and unconfined aquifer case studies. It is found that for both cases, the CIP-method is superior in terms of calculation time while keeping an acceptable numerical accuracy.     

氨氮实验室空白偏高的影响因素研究

利用排除法对影响氨氮实验室空白测定的各种因素进行了考察。结果表明,固定剂硫酸的添加不会引起空白值偏高。滤纸因含有铵盐会引起空白偏高,但可采取用去离子水浸泡的方法消除。絮凝沉淀过程中应避免将水体pH调至9.0左右。在水体pH=9.0左右时,沉淀物颗粒尺寸最小,过滤时渗入滤后液中,影响吸光度;过滤后的滤液pH会降低,导致滤液中重新析出沉淀物,也影响吸光度。     

Atmospheric Aerosol over a Southeastern Region of Texas: Chemical Composition and Possible Sources

Speciated samples of PM_2.5 were collected at a site in Jefferson County, Texas by US EPA (Environmental Protection Agency) from July of 2003 to August of 2005. A total of 269 samples with 52 species were measured; however, 22 species were excluded in this study because of too many below-detection-limit data. The data set was analyzed by positive matrix factorization (PMF) to infer the sources of PM observed at the site. The analysis identified ten sources: sulfate-rich secondary aerosol I (35.9%), sulfate-rich secondary aerosol II (21.0%), cement/carbon-rich (11.7%), wood smoke (8.8%), metal processing (6.3%), motor vehicle/road dust (5.7%), nitrate-rich secondary aerosol (3.3%), soil (3.2%), sea salt (2.6%), and chloride depleted marine aerosol (1.6%). Sulfate and nitrate mainly exist as salts. The two sulfate-rich secondary aerosols account for almost 57% of the PM_2.5 mass concentration. The factor containing highest concentrations of Cl and Na was attributed to sea salt due to the proximity of the monitoring site to the Gulf of Mexico. The chloride depleted marine aerosol was related to the sea salt aerosol. Cement/carbon-rich, wood smoke, metal processing, and motor vehicle/road dust factor were likely to be the local sources.