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991.
992.
本文以塔里木盆地为例,通过流体势分析,油田水化学分析,包裹体测温和原油中含氮化合物的丰度及比值研究,确定塔中地区晚海西期油气主要来自东北和西北两个方向,在中段形成塔中4油藏,并通过流体运移方向分析,认为塔中4油藏在喜马拉雅期受淡水冲洗破坏,使油所储量大大减少,轮南地区的油气主要来自南部的满加尔凹陷和两侧的哈拉哈塘凹陷和草湖凹陷,其中草湖凹陷两次供油气,而其他两个凹陷三次供油气,流体运移方向的研究有助于认识油气的分布规律,对确定勘探的有利区带和目标具有重要意义。 相似文献
993.
Munendra Singh 《Environmental Geology》2001,40(6):664-671
The Yamuna River sediments, collected from Delhi and Agra urban centres, were analysed for concentration and distribution
of nine heavy metals by means of atomic adsorption spectrometry. Total metal contents varied in the following ranges (in mg/kg):
Cr (157–817), Mn (515–1015), Fe (28,700–45,300), Co(11.7–28.4), Ni (40–538), Cu (40–1204), Zn (107–1974), Pb (22–856) and
Cd (0.50–114.8). The degree of metal enrichment was compared with the average shale concentration and shows exceptionally
high values for Cr, Ni, Cu, Zn, Pb and Cd in both urban centres. In the total heavy metal concentration, anthropogenic input
contains 70% Cr, 74% Cu, 59% Zn, 46% Pb, 90% Cd in Delhi and 61% Cr, 23% Ni, 71% Cu, 72% Zn, 63% Pb, 94% Cd in Agra. A significant
correlation was observed between increasing Cr, Ni, Zn, and Cu concentrations with increasing total sediment carbon and total
sediment sulfur content. Based on the Müller's geoaccumulation index, the quality of the river sediments can be regarded as
being moderately polluted to very highly polluted with Cr, Ni, Cu, Zn, Pb and Cd in the Delhi and Agra urban centres. The
present sediment analysis, therefore, plays an important role in environmental measures for the Yamuna River and the planning
of these city centres.
Received: 21 June 1999 · Accepted: 1 October 1999 相似文献
994.
张家界地区中晚寒武世岩相带3分格局明显,自NW向SE依次为台地相、台缘斜坡相和陆棚相。3相区之间分别以花坦-张家界、古丈-张家界深大断裂为界。台地相欧孔王溪组属邻近盆缘陡坡地带类似于深水陆棚沉积,重力沉积发育;娄山关组北西小区记录了由台地边缘浅滩→局限台地潮坪→台地边缘浅滩的变迁过程;而东南小区则属台地边缘与斜坡的过渡地带。台缘斜坡相区敖溪组反映了缓慢的海退过程,沉积环境由陆棚向陆棚内缘带变迁;车夫组属台地前缘斜坡带,重力沉积转化为蚀流沉积;比条组为背景沉积综合产物,反映了台地前缘斜坡上带环境,陆棚相区探溪组旋回性明显。反映了陆棚内缘沉积特点;田家坪属台缘斜坡下带-陆棚内缘环境,沉积了一套多具鲍玛层序的远源风暴岩。各自有其岩石类型组合特征及沉积构造特征,并讨论了岩相古地一的演化规律。 相似文献
995.
利用激光拉曼探针测定了单个流体包裹体成分 ,计算了流体的 pH、Eh值 ,并从不同角度对大港探区的油气运聚规律和储层评价进行应用研究。结果表明 ,本研究区表现出具明显的两期 (早、晚 )油气运聚特征。还对油气资源进行了评价 ,展现了流体包裹体研究方法在油气运聚规律研究中具有良好的应用与发展前景 相似文献
996.
胶州湾养殖海区沉积物中酸可挥发性硫的研究 总被引:19,自引:1,他引:19
沉积物中酸可挥发性硫化物(AVS)的含量对控制重金属在沉积物/间隙水中的分配和重金属的生物可利用性方面有重要意义,也是海洋养殖业的重要指标之一,研究改正目前《海洋监测规范》中沉积物酸可挥发硫化物的测定方法基础上,建立了一套简单易行的仪器装置和分析程序,讨论了N2流量、反应时间、酸强度、硫总量4个方面对测定结果的影响,给出了胶州湾海区沉积物中AVS的定量数据,表明胶州湾养殖海区沉积物中AVS的含量显著高于非养殖海区和其它海湾沉积物中AVS的定量数据,表明胶州湾养殖海区沉积物中AVS的含量显著高于非养殖海区和其它海湾沉积物中AVS的含量,探讨了应用AVS归一化沉积物中二价有毒金属评价其化学活性和生物可用性的可能性。 相似文献
997.
In-stream wetlands and their significance for channel filling and the catchment sediment budget, Jugiong Creek, New South Wales 总被引:2,自引:0,他引:2
Evidence is presented here of recent and extensive infilling of the incised channel network of the Jugiong Creek catchment, SE Australia. The present channel network resulted from widespread stream and gully incision in the period between 1880 and 1920. Our survey shows that gully floors have been colonised extensively by emergent macrophyte vegetation since before 1944, forming continuous, dense, in-stream wetlands, which now cover 25% of the channel network in the 2175 km2 catchment and have so far trapped almost 2,000,000 t of nutrient-enriched, fine sediments. This mass of sediments represents the equivalent of 4.7 years of annual sediment production across the catchment and in some tributaries, more than 20 years of annual yield is stored within in-stream wetlands.Previous work on the late Quaternary stratigraphy of the region has shown that there were repeated phases of channel incision in the past following which the channels quickly stabilised by natural means and then filled with fine-grained sediment to the point of channel extinction, creating unchannelled swampy valley floors. The current formation and spread of in-stream wetlands is interpreted to be the onset of the next infill phase but it is not known whether present conditions will allow complete channel filling and reformation of the pre-existing swampy valley floors. Nevertheless, further spread of in-stream wetlands is likely to increase the sediment trapping capacity and further reduce the discharge of sediments and nutrients into the Murrumbidgee River. The in-stream wetlands may provide a significant capacity to buffer erosion from gullied catchments of considerable size (up to 300 km2) as an adjunct to current riparian management options. They may also assist the recovery of sediment-impacted channels downstream. 相似文献
998.
999.
1000.
Denise J. Reed 《地球表面变化过程与地形》1995,20(1):39-48
In order to maintain an elevation in the intertidal zone at which marsh vegetation can survive, vertical accretion of the marsh surface must take place at a rate at least equal to the rate of relative sea-level rise. Net vertical accretion of coastal marshes is a result of interactions between tidal imports, vegetation and depositional processes. All of these factors are affected, directly or indirectly, by alterations in marsh hydrology which might occur as a result of sea-level rise. The overall response of coastal marshes to relative sea-level rise depends upon the relative importance of the inorganic and organic components of the marsh soil and the impact of increased hydroperiod on net accumulation. The varied combination of factors contributing to sediment supply, and their complexity at the scale of individual marshes, means that predicting the response of suspended sediment concentration in marsh floodwater to any changes which may occur as a result of sea-level rise, at anything other than the local scale is unlikely to be accurate. The impact of sea-level rise on net below-ground production is also complex. The sensitivity of certain species to waterlogging and soil chemical changes could result in a change in species composition or the migration of vegetation zones. Consequently, predicting the net impact of sea-level rise on organic matter accumulation is fraught with difficulties and requires improved understanding of interactions between vegetation, soil and hydrologic processes. 相似文献