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1.
邻二氮菲分光光度法测定碳酸盐相中微量亚铁   总被引:2,自引:2,他引:2  
建立了在超声波作用下,HAc—NaAc缓冲溶液和邻二氮菲选择性溶解分光光度法直接测定碳酸盐相中微量亚铁的方法。结果表明,在适宜条件下,含2g/L邻二氮菲的HAc—NaAc缓冲溶液(pH3)可选择性溶解并络合碳酸盐相中的Fe(Ⅱ),通过加入EDTA溶液有效地抑制了Fe(Ⅲ)的光还原作用。常见含铁矿物如赤铁矿、磁铁矿及硅酸盐等均对碳酸盐中Fe(Ⅱ)的测定无干扰。样品经30%的H2O2浸泡、过滤、晾干预处理,能有效地消除黄铁矿和有机物的干扰。方法用于石灰岩国家一级标准物质的测定,结果与标准值相符。  相似文献   
2.
对处于蠕滑阶段的边坡而言,准确确定蠕滑段和锁固段是进行稳定性评价及演化趋势预测的基础和前提。以我国西南山区某水库型岸坡变形体为例,在综合分析岸坡工程地质条件的基础上,通过联合运用野外现场地质调查、地表位移监测、钻孔、平硐、深部位移监测、物探等多种勘察手段,查明了岸坡的结构特征,并分别对岸坡进行地表和深部变形分区。 在此基础上,结合当前稳定性现状,划分出岸坡蠕滑段与锁固段。结果表明:(1)岸坡在河谷下切过程中发生了弯曲倾倒变形,弯曲折断面深度为20~80m;(2)岸坡前部为蠕滑段,中部为锁固段,后部为拉裂段,具备滑移-拉裂-剪断三段式发育特征。研究结果可直接用于该岸坡变形体的稳定性评价,且对于同类型处于蠕滑阶段边坡的勘察手段及综合分析具有一定的借鉴意义。  相似文献   
3.
This study investigates urbanization and its potential environmental consequences in Shanghai and Stockholm metropolitan areas over two decades. Changes in land use/land cover are estimated from support vector machine classifications of Landsat mosaics with grey-level co-occurrence matrix features. Landscape metrics are used to investigate changes in landscape composition and configuration and to draw preliminary conclusions about environmental impacts. Speed and magnitude of urbanization is calculated by urbanization indices and the resulting impacts on the environment are quantified by ecosystem services. Growth of urban areas and urban green spaces occurred at the expense of cropland in both regions. Alongside a decrease in natural land cover, urban areas increased by approximately 120% in Shanghai, nearly ten times as much as in Stockholm, where the most significant land cover change was a 12% urban expansion that mostly replaced agricultural areas. From the landscape metrics results, it appears that fragmentation in both study regions occurred mainly due to the growth of high density built-up areas in previously more natural/agricultural environments, while the expansion of low density built-up areas was for the most part in conjunction with pre-existing patches. Urban growth resulted in ecosystem service value losses of approximately 445 million US dollars in Shanghai, mostly due to the decrease in natural coastal wetlands while in Stockholm the value of ecosystem services changed very little. Total urban growth in Shanghai was 1768 km2 and 100 km2 in Stockholm. The developed methodology is considered a straight-forward low-cost globally applicable approach to quantitatively and qualitatively evaluate urban growth patterns that could help to address spatial, economic and ecological questions in urban and regional planning.  相似文献   
4.
安徽南部地区金矿控矿条件及其成矿规律研究   总被引:1,自引:1,他引:0  
安徽省金矿床(点)主要集中于其南部地区,金多以共生或伴生形式产在铜、铁、硫矿床中,中大型金矿床少,独立的岩金矿更少。前人对安徽南部地区开展了大量针对铜、铁、硫等矿床地质地球化学及其成因上的研究,而对独立的岩金矿床则鲜有研究。本文通过对该区独立岩金矿床金成矿地质背景介绍,对区内铜陵朝山、铜陵杨冲里、南陵吕山、池州抛刀岭、休宁天井山等代表性金矿床特征总结归类,对与金成矿相关的地层、构造及岩浆岩等控矿条件进行了梳理和分析研究,同时对区域金矿床时间和空间分布规律特征进行了探讨归纳,从而将安徽南部地区独立金矿床大致划分为五种成因类型,并指出该区金成矿主体发生在燕山早期,受中生代太平洋板块俯冲和俯冲后拉张双重作用影响,同时金成矿主要与早期俯冲阶段有关,晚期则叠加了少量金及多金属矿种,是燕山期中国东部构造体制转换与成矿大爆发事件具体体现和响应。含金流体主要富集在由晋宁期基底基础上演化而来断裂构造中或岩体与围岩接触带上,大致具有北东向、北东东向集中展布的特征。通过上述工作,以期为今后在该地区开展与金矿床相关的野外地质工作及科研工作者提供借鉴,进而为该地区金矿取得找矿突破提供指导和理论基础。  相似文献   
5.
湘东-赣西NNE向走滑断裂与地震、地热关系   总被引:4,自引:0,他引:4  
该文重点研究了湘东、赣西地区NNE向活动走滑断裂系与地震和温泉分布之间的密切联系。结果表明:①研究区地震和温泉主要集中在3条NNE向主走滑断裂带及及伴生的P、P’断裂带;②高温热泉或强震震中区的基本构造样式为走滑断层左行、左阶雁列带和拉分盆地构造;③陆壳结构分层特征是影响该区地震作用强度的一个重要因素。  相似文献   
6.
For low-slope hilly land development to have more new land space in a watershed, it is particularly important that to coordinate the sharply increasing conflicts between mountainous and urban land utilization in the city. However, development of low-slope hilly land easily induce potential risks of geologic hazards such as landslide and landslip. It may lead to further environmental losses in a watershed. Hence, it is necessary to study potential risks of geo-hazards in low-slope hilly land development in urban area. Based on GIS spatial analysis technique, we select a study area, Dali City in the Erhai Basin located in watershed belt of Jinsha River, Lancang River and Red River in Yunnan Province of China. Through studying some relevant key indexes and parameters for monitoring potential risks of geo-hazards, we establish a composite index model for zoning the area with potential risks of geo-hazards in development of low-slope hilly land in the study area. Our research findings indicate that the potential risks of geo-hazards in eastern Dali City is relatively low while of that on slow hills with gentle slopes in the western area are relatively high. By using a zoning research method, generated maps show geological information of potential risks of geo-hazards on low-slope hilly land which provide important messages for guarding against natural geo-hazards and potential environmental losses in a watershed.  相似文献   
7.
《Quaternary Science Reviews》2003,22(5-7):703-723
The Western Siberian lowlands (WSL) are the world's largest high-latitude wetland, and possess over 900,000 km2 of peatlands. The peatlands of the WSL are of major importance to high-latitude hydrology, carbon storage and environmental history. Analysis of the existing Russian data suggests that the mean depth of peat accumulation in the WSL is 256 cm and the total amount of carbon stored there may exceed 53,836 million metric tons. A synthesis of published and unpublished radiocarbon dates indicates that the peatlands first developed at the end of the Last Glacial, with a rapid phase of initiation between 11,000 and 10,000 cal yr BP. Initiation slowed after 8000 cal yr BP and reached a nadir at 4000 cal yr BP. There has been renewed initiation, particularly south of 62°N, following 4000 cal yr BP. The initial development of peatlands in the WSL corresponds with the warming at the close of the Pleistocene. Cooling after 4000 Cal yr BP has likely led to increased permafrost and increased peatland development particularly in central and southern regions. Cold and dry conditions in the far north may have inhibited peatland formation in the late Holocene.  相似文献   
8.
在长江中游湖北省东部网湖湖心的采取柱状沉积物,用210Pb+137Cs方法测定表层的沉积速率.制作连续切片,选取深度7烈-88lmm的层型沉积较完整的一段样品,用显微镜量测浅色层和暗色层的厚度,采用电子探针确定层的地球化学成份,并由此计算了纹层的主要矿物组成.认为纹层主要是由于在洪水季节长江带来的浅色泥沙与在枯水季节富水河带来的含暗色矿物泥沙交替沉积形成的.泥沙主要来源于夏季长江倒灌入湖的洪水,部分来自长江支流富水河;冬季枯水季节,泥沙基本来源于长江支流富水河.  相似文献   
9.
晏鄂川  王明华  余子华 《岩土力学》2006,27(Z1):643-647
三峡库区某岩质滑坡的变形失稳涉及到地质、环境、人类工程活动等多种因素。针对该滑坡的变形破坏规律和诱发机制,拟采用削坡、抗滑桩、排水系统等加固措施,以确保滑坡整体和局部稳定,其中加固方案的长期有效性将是整个治理工程的关键。通过对大变形数值方法以及滑坡治理工程措施特点的分析,认为在研究滑坡治理工程大变形问题时采用非线性大变形数值方法更加合理,加固方案的优化设计采用了三维快速拉格朗日分析(FLAC3D)法,通过对滑坡区位移场以及破坏区的变化规律进行分析,将各项加固措施及其组合工况的治理效果进行对比优选,最后确定出以抗滑桩和削坡为主、排水为辅的最优加固方案。该方案的治理效果已被实践资料所证实,其中的部分方法和结论对三峡库区滑坡地质灾害的防治具有指导意义。  相似文献   
10.
The aim of this paper is to quantify the socioeconomic impacts of hydropower development to reflect its positive functions from multiple perspectives and dimensions. By applying the multi-regional Computable General Equilibrium (CGE) model to a case study of the Yibin–Chongqing section along the upper reaches of the Yangtze River, the analysis shows that hydropower development has outstanding benefits for the regional economy and livelihood improvement, as proved by various indicators including consumption, investment, GDP, employment, and income. Meanwhile, application of the CGE model provides an effective way to quantitatively assess the socioeconomic impact of hydropower and other clean energy development.  相似文献   
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