海陆边缘沉积磷在全球变化研究中的意义   总被引：9，自引：1，他引：8  

翁焕新 《地球科学进展》1999,14(5):524-528

从磷的生物地球化学循环的角度,讨论了磷与大气圈O2、CO2的关联模式,并通过研究磷的环境地球化学行为,揭示了海陆边缘沉积磷对古气候、古环境变化的记录及其对指示古全球变化的关键性,同时提出了中国东部沿海近代沉积磷的积累与全球变化的耦合作用关系,在中短时间尺度的全球变化研究中所具有的特殊意义。  相似文献   

川南煤系硫铁矿矿山地质环境现状分析   总被引：1，自引：0，他引：1  

蒋俊 《四川地质学报》1999,(4)

着重分析当前川南煤系硫铁矿的矿山地质环境现状,以及硫铁矿山普遍存在的一些地质环境问题,旨在引起社会各方面对矿山地质环境保护的重视。  相似文献   

颗石藻与海洋、环境关系之探讨   总被引：3，自引：0，他引：3  

侯奎  陈镇东 《化工矿产地质》1999,21(1):31-39

笔者在20年的研究中相继发现,自中元古代和古生代以来海相钙质超微浮游生物－颗石藻的新属种达180余种,通过对颗石藻在海洋中分布状态与固碳特征的研究,证明颗石藻乃是海洋中重要的基础生产者,它和海洋碳酸盐及相关生物存在着密切的关系,其能借助光合作用,吸收海水中的CO2,而释放出氧气．对减少全球温室效应与保护地球生态环境平衡,有相当重要的贡献。  相似文献   

A geo-environmental map for the sustainable development of the Kathmandu Valley, Nepal     

Omkar M. Shrestha  Achyuta Koirala  Jörg Hanisch  Klaus Busch  Martin Kerntke  Stefan Jäger 《GeoJournal》1999,49(2):165-172

An engineering and environmental geological map of the Kathmandu Valley in Nepal has been elaborated within a project of German-Nepalese cooperation. In the Kathmandu Valley, the major geo-environmental problems arise from haphazard exploitation of geologic resources, local landslide zones, severe problems of garbage disposal, river flooding and a dramatic river pollution. The map was prepared by the use of GIS techniques. It contains all basic geological and environmental data, as geotechnical risk zones (landslide-prone areas or those of poor foundation conditions), areas for preferable extraction of construction material and those not to be allowed to be exploited, areas of immediate need of reforestation in order to prevent landslide or badland development, groundwater protection zones, and suitable garbage disposal sites. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献   

湖泊环境科学钻探施工技术   总被引：7，自引：1，他引：6       下载免费PDF全文

刘宝林  何跃文  司敬成 《探矿工程》1999,(2):47-49

针对内蒙古岱涨的施工条件和湖底沉积物的类型,对湖泊环境科学钻探技术进行了讨论,从钻探取心角度,将岱海沉积物分为４种有代表性的地层;提出了每种地层中可能遇到的技术问题对使用的取心钻具的效果进行了评价,并提出了合理化改进意见,总结了湖泊钻进工艺方法;给出了简易钻探平台的拼装方式和主要钻探设备的性能;探讨了湖泊钻探的发展前景和进一步工作计划。  相似文献   

RIVERS' FEATURES ON ALLUVIAL FANS IN NORTHWEST CHINA     

ZHU Zhongli  MO Duowen 《国际泥沙研究》1999,(2)

IINTRODUCTIONAlluvialfanisakindofsedimentogeniclandform,whichisdevelopedwhereriverflowsoutofmountain.Holdingapositionalongfootsofmostmountains,itconstittltestheimportantpartofthefluvialsedimentarysystem.Hooke(1967)describedtraditionalriverformonalluvialfans.Riversinciseandformdeepstableandunstablechannelsonupperpartsofalluvialfans.Andbelowtheintersectionpoints,riversflowoutofthevalleysinformofbraidedchannelanddepositsmallsecondaryajlluvialfansonthesurfaceofthefan.Lobeck(1939,fromRochocki…  相似文献   

Facies architecture of an isolated carbonate platform: tracing the cycles of the Latemàr (Middle Triassic, northern Italy)     

Sven O. Egenhoff  Arndt Peterhänsel  Thilo Bechstädt  Rainer Zühlke  & Jürgen Grötsch 《Sedimentology》1999,46(5):893-912

The 720-m-thick succession of the Middle Triassic Latemàr Massif (Dolomites, Italy) was used to reconstruct the lagoonal facies architecture of a small atoll-like carbonate platform. Facies analysis of the lagoonal sediments yields a bathymetric interpretation of the lateral facies variations, which reflect a syndepositional palaeorelief. Based on tracing of lagoonal flooding surfaces, the metre-scale shallowing-upward cycles are interpreted to be of allocyclic origin. Short-term sea-level changes led to subaerial exposure of wide parts of the marginal zone, resulting in the development of a tepee belt of varying width. Occasional emergence of the entire lagoon produced lagoon-wide decimetre-thick red exposure horizons. The supratidal tepee belt in the backreef area represented the zone of maximum elevation, which circumscribed the sub- to peritidal lagoonal interior during most of the platform's development. This tepee rim, the subtidal reef and a sub- to peritidal transition zone in between stabilized the platform margin. The asymmetric width of facies belts within individual metre-scale cycles was caused by redistribution processes that reflect palaeowinds and storm paths from the present-day south and west. The overall succession shows stratigraphic changes on a scale of tens of metres from a basal subtidal unit, overlain by three tepee-rich intervals, separated by tepee-poor units composed of subtidal to peritidal facies. This stacking pattern reflects two third-order sequences during the late Anisian to early middle Ladinian.  相似文献   

厦门寨后垃圾填埋场释气影响及其控制   总被引：2，自引：0，他引：2  

蔡榕硕  姚瑞梅  杜华晖 《台湾海峡》1999,18(4):474-480

本文是在承担厦门市寨后“垃圾埋场”工程环境影响评价的基础上,对该填埋场的垃圾释气规律作进一步研究。研究结果表明,（１）厦门煤气的普及率较高;（２场营运１１ａ左右,废气产物量及排一达到最大值;（３）于小风条件下,在下风向５０ｍ处,ＣＨ４浓度可达爆炸极１６￣３１％,所产生的恶臭气体Ｈ２Ｓ的影响距离经ＮＨ３大,在下风向５００ｍ下才能达到２级场界标准;（４）严格按卫生填埋的技术标准进行规范操作,确保排气管  相似文献   

Direct Measurements of Deep Currents in the Northern Japan Sea   总被引：5，自引：0，他引：5  

Masaki Takematsu  Zentaro Nagano  Alexander G. Ostrovski  Kuu Kim  Yuri Volkov 《Journal of Oceanography》1999,55(2):207-216

Long-term current measurements by means of subsurface moorings were made for the first time at seven sites in the Japan Basin, the northern part of the Japan Sea. The objective was to directly explore the velocity field in the highly homogeneous deep water mass (the Japan Sea Proper Water) that occupies depths below 500 m. On each mooring three current meters were equipped at an approximately equal distance below about 1000 m depth. Duration of the measurements was 1 to 3 years depending on specific site. This paper describes the basic data set from the moored measurements. It is found that the deep water of the Japan Basin is very energetic with eddies and vertically coherent currents of the order of 0.1 m/s. Surprisingly, the currents and eddies exhibit strong seasonal dependence even in the deepest layers of the Basin. The observed new current features are discussed in comparison with conventional deep circulation pictures derived from hydrographic data. This revised version was published online in August 2006 with corrections to the Cover Date.  相似文献   

Holocene environmental change according to lake core in Fildes Peninsula of King George Island,Antarctica     

李小梅  袁宝印  赵俊琳 《极地研究(英文版)》2002,13(2)

Lake core sampled from Xihu in Fildes Peninsula of King Gorge Island, Antarctica could reveal the environmental change of the district. The lake core( GA7) , 9.28 meters long , was sectioned at an interval of 2 cm. Through measuring the organic carbon, magnetic susceptibility, granularity and organic carbon isotope of GA7, by use of 14C age it was estimated that there were four periods of high temperature in Fildes Peninsula; 4800-4400 aB. P. , 3600-3350 aB. P. ,2100 - 1800 aB. P. and 900 aB. P. - present. Meanwhile, results showed that there was a strikingly positive correlation between the content of organic carbon and that of organic carbon isotope (δC01213 ) which could be the substitute indicators of environmental temperature.  相似文献