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991.
In this study two sites were selected in order to investigate groundwater contamination and spatial relationships among groundwater quality, topography, geology, landuse and pollution sources. One site is the Asan area, an agricultural district where pollution sources are scattered and which is mainly underlain by granite of Cretaceous age. The other site is the Gurogu area of Seoul city, an industrial district where an industrial complex and residential areas are located and which is mainly underlain by gneiss of Precambrian age. Groundwater samples collected from these districts were analysed for chemical constituents. An attribute value files of chemical constituents of groundwater and the spatial data layers were constructed and pollution properties were investigated to establish out spatial relationships between the groundwater constituents and pollution sources using geographic information systems (GIS).Relatively high contents of Si and HCO3 in the groundwater from the Asan area reflect the effect of water–rock interaction whereas high contents of Cl, NO3 and Ca2+ in the groundwater from the Gurogu area are due to the pollution of various sources. The significant seasonal variation of SiO2, HCO2 and Ca2+ contents, and that of Ca2+ content were observed in the Asan and the Gurogu areas, respectively. Seasonal variation of pollutants such as Cl, NO3 and SO4 2– was not observed in either area. Pollution over the critical level of the Korean drinking water standard has been investigated from 15 sampling sites out of 40 in the Asan area, and 33 sampling sites out of 51 in the Gurogu area. Pollution by NO3 , Cl, Fe2+, Mn2+, SO4 2– and Zn2+ in the groundwater from the industrial district (Gurogu area) and that of NO3 , SO4 2– and Zn2+ in the groundwater from the agricultural district (Asan area) were observed. The principal pollutant in both areas is NO3 . Deep groundwater from the Asan area is not yet contaminated with NO3 except for one site, but most of the shallow groundwater site occurring near the potential point sources is seriously contaminated. From the result of buffering analysis, it seems clear that factories and stock farms are the principal pollution sources in the Asan area. The groundwater from the Gurogu area has already been seriously polluted considering the fact of NO3 contamination of deep groundwater. Chlorine pollution of shallow groundwater in the Gurogu area was also observed. Spatial relationship between pollution level and its source was clarified in this study by using GIS, which will be applicable to the effective management of groundwater quality.  相似文献   
992.
九龙江口桐花树红树林对重金属的吸收与累积   总被引:19,自引:0,他引:19  
探讨了福建九龙江口桐花树红树林对CU、Ph、Zn、Cd、Mn元素的吸收、累积及分布.结果表明:该林地土壤5种元素的储量关系为Mn>Zn>Ph>CU≥Cd;植物体不同部位,各元素含量有着明显的差异,含量范围分别为Ch1.51~5.70、Pb1.30~10.70、Zn18.0~100.1、Cd0.04~0.23和Mn15.5~237.5(w/10-6);植物对土壤元素的富集系数大小依次为Cd>Zn>Mn>Cu>Ph;群落现存生物量中,CU、Pb、Zn、Cd、Mn元素的现存累积量分别为16.56、63.30、445.05、1.14和1656.93(ρA/mg·m-2).其中,地下部分别占70.2%、81.8%、76.2%、72.2%和82.1%;林地残留物相应元素的储量分别为211.11、184.00、1941.69、6.19和22248.31(ρA/μg·m-2).  相似文献   
993.
论述了高校运用责任会计进行财务管理工作的必要性及其可能性,提出了高校财务管理应用责任会计的某些构想,最后指出了高校全面推行责任会计存在的几个问题。  相似文献   
994.
广西山地漂白黄壤分布在中、低山地的上部,即海拔1200m以上的山体坡面和山顶部位,成为广西土壤垂直带谱最上层结构的主要土壤类型.在温暖多雨、多云雾的亚热带季风气候条件下,以常绿阔叶林为主的自然森林植被生长茂密,土壤矿物分解较为彻底,成土过程主要是旺盛的生物富集过程、明显的脱硅富铅化与水化过程以及强烈的淋浴侧渗漂洗过程。土壤剖面层次发育明显,具A1-A2-E-B-C或AH-A-E-B-C构型。土壤质地多为重壤土至中粘土,呈强酸性反应。表土阳离子代换量中等,有机质含量丰富,肥力高,适于发展林业,特别是发展水源林和水土保持林,它是广西最重要的水源林区。  相似文献   
995.
珠江三角洲经济区耕地锐减,水资源分布不均,工业和农业污染严重,农业生态环境日趋恶化。经济发展不平衡,农业趋于萎缩状态,本文针对这些问题,提出了珠江三角洲农业生态环境治理的指导思想、发展目标和基本措施。  相似文献   
996.
太行山是我国山地植被破坏历史最长、生态环境严重恶化的山地生态系统,“七五”期间国家将绿化太行山列入重点攻关项目。从1986年开始,作者根据生态工程原理提出:环境辨识工程、种群引进选择工程、种群匹配工程、水土富集工程、时间节律工程和食物链工程为主的立体林业工程新思想,并在湘山小流域建起实施模式。经四年的工作,已取得较大进展。  相似文献   
997.
本项调控工程分两步:1984—1986年在山一村106ha农田开展病虫害综合防治试验示范;1987—1989年将试验成果应用于生产。试验研究取得了明显的经济效益、生态效益和社会效益:农药用量比1983年前减少80.6%,稻谷中农药残留不超标(原有机氯农药666残留超标率31.6%);害虫天敌稻田蜘蛛增加83.3—180.0%,稻虱多索线虫增加2倍;防治农药成本减少53.7%。并制定了《山一村农田农药污染防治技术规程》,其主要内容有:开展病虫害“二查二定”,达到防治指标时用药;制定病虫害防治策略,在防治适期内用药;推广高效低残留农药,遵守农药安全间隔期;推广抗性良种,适施N肥,增施P、K肥;保护利用天敌,发挥天敌自然抑制作用。  相似文献   
998.
本文从灾害的概念及其发展入手,分析了农村生态经济系统发生灾变的原因,提出了减轻或防止农村生态经济系统灾变的有效对策。文章对合理调控农村生态经济系统,实现农村生态经济平衡,防止或减轻农村灾害发生等问题作了比较深入的研究。  相似文献   
999.
在脱硫脱硝喷淋装置上采用氨法-络合法处理工业烟气。考察了吸收液pH、Fe(Ⅱ)EDTA浓度、初始烟气浓度、液气比对烟气同时脱硫脱硝效果的影响。实验结果表明:吸收液的酸碱度通过影响Fe(Ⅱ)与EDTA的络合形式进而影响NO去除率;SO_2去除率主要受吸收液pH和初始SO_2质量浓度的影响;当吸收液pH大于8、吸收液Fe(Ⅱ)EDTA浓度大于0.100 mol/L、初始SO_2质量浓度小于1 500 mg/m3、初始NO质量浓度为1 200 mg/m3时,SO_2去除率均在95%以上,NO去除率为54%;当液气比由1 L/m3增大至4 L/m3时,有效脱硫时间和有效脱硝时间分别增长了7 min和4 min。  相似文献   
1000.
Soil translocation for recultivation of soil removed from construction sites and for the preparation of refilled lysimeters inevitably involves disturbance of soil structure, and, if intermediate storage is included, also drying and rewetting of the soil. We report on an experiment with model forest ecosystems, where uncontaminated forest subsoils were covered with non-contaminated or freshly heavy metal (mainly Zn and Cu) contaminated topsoil in large lysimeters. Monitoring of the chemical composition of the drainage water revealed two distinct soil conditioning phases. During an initial phase of about a year strongly elevated nitrate and sulfate concentrations occurred that were attributed to a mineralisation flush caused by the increased accessability of mineralisable nitrogen and sulfur in destroyed aggregates. These effects were significantly larger in lysimeters with calcareous subsoil than in those with acidic subsoil. The second phase was characterised by a gradual decrease in dissolved organic carbon and sulfate concentrations, in particular in the acidic subsoil. This decrease may be attributed to the depletion of pools made accessible during aggregate destruction or the formation of new aggregates. These chemical changes had only little effects on the concentrations of copper and zinc in the drainage water. Based on our results, it can be concluded that large refilled lysimeters can be used for many purposes without risk of compromised results, if a conditioning phase of about 1 year with sufficiently moist soil conditions is respected. Nevertheless, gradual changes in soil chemical characteristics still occur after this initial phase. Implications for the recultivation of sites using relocated soils are discussed.  相似文献   
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