西藏高原对其北方环流系统的影响     

杨鉴初  汪关成  李玉兰 《气象学报》1959,30(1):99-113

本文应用1956年6月到1957年5月一年内逐日亚欧500mb 天气图,计算历次高低压系统经过西藏高原以北时在强度和速度方面的改变,证明这些改变是有规则的,在地域上和季节上皆表现出独特性。  相似文献   

北半球海平面气压场月偏距中心的研究     

杨鉴初  李玉兰 《气象学报》1959,30(4):297-305

本文用统计方法研究1930—1939年期间逐月北半球气压偏距中心的活动规律.发现同一月份的气压偏距中心在北半球某些地区有集中出现的情况,这些集中地区如在阿拉斯加的南方、大西洋的东北部以及亚欧大陆的北冰洋沿岸.这些地区可以认为是北半球环流异常的关鍵性地区.绝大多数的偏距中心在逐月之间可以发现它们的联系.在过渡季节,大多数偏距中心自西向东移动.在偏距中心相互作用的基础上,本文还讨论了北半球某些地区的气候特点.  相似文献   

A SURVEY OF HIGH RESOLUTION GEOMAGNETICS *     

LEE LANGAN 《Geophysical Prospecting》1966,14(Z2):488-503

The development of optically pumped and monitored “atomic” magnetometers has allowed the application of greater resolution in geomagnetic measurements for exploration purposes. This paper presents a survey of instrumentation in use, the variety of exploration techniques that are being used in practice, and an estimate of their state of development. Alkali metals (rubidium and cesium) and helium have been used as active elements to obtain the magnetic-field dependent Larmor frequency. Each of these instruments is capable of obtaining high resolution data (data with sensitivity numerically smaller than one-tenth gamma). They have been adapted for airborne, land, and marine usage. Such sensitivity has enabled the rapid development of geomagnetic gradiometers, high sensitivity aeromagnetics, diurnally reduced ground surveys, broad-band magneto-telluric surveys, susceptibility measurements, and convenient magnetic search and location techniques. Outlines of each procedure and an example of its application are given.  相似文献   

LANDSLIDE POTENTIALITY OF THE TSENGWEN RESERVOIR WATERSHED, TAIWAN     

Chin-yu LEE Professor  Department of Soil  Water Conservation  National Pingtung University of Science  Technology  Pingtung    Taiwan  R.O.C. 《国际泥沙研究》2004,(2)

To recognize the geographical characteristics of the landslide areas will be helpful for the watershedmanagement in the reservoir watershed. According to the quantitative analysis, we'll take differentscores and weighting for the potential parameters of the landslide areas in the Tsengwen reservoirwatershed, and in the meanwhile, we'll extract the different factors, including the slope, aspect,altitude, soil and geological textures etc., and the results shown as maximum one--day rainfall, ratio offorests and average relief is the most affecting parameters on the potential risk map of landslide areas.  相似文献   

Prediction analysis of long-term memory effect for calamity gray series     

CHEN Zhaonan 《中国科学D辑(英文版)》2004,47(3)

Are human able to foresee the future? For thou-sands of years close attention has been paid to this issue. At the present day, in order to survive from competition and to predominate over the nature, hu-man抯 desire of forecasting things has become more and more intense. Compared to conquering space, more people yearn for being able to control the time. From ancient to the present, mankind always dream of contacting the past, governing the present and tran-scending the future. Recent years in…  相似文献   

Similar V/Sc Systematics in MORB and Arc Basalts: Implications for the Oxygen Fugacities of their Mantle Source Regions   总被引：8，自引：0，他引：8  

AEOLUS LEE  CIN-TY; LEEMAN  WILLIAM P.; CANIL  DANTE; LI  ZHENG-XUE A 《Journal of Petrology》2005,46(11):2313-2336

V/Sc systematics in peridotites, mid-ocean ridge basalts andarc basalts are investigated to constrain the variation of fO₂in the asthenospheric mantle. V/Sc ratios are used here to ‘seethrough’ those processes that can modify barometric fO₂determinations in mantle rocks and/or magmas: early fractionalcrystallization, degassing, crustal assimilation and mantlemetasomatism. Melting models are combined here with a literaturedatabase on peridotites, arc lavas and mid-ocean ridge basalts,along with new, more precise data on peridotites and selectedarc lavas. V/Sc ratios in primitive arc lavas from the Cascadesmagmatic arc are correlated with fluid-mobile elements (e.g.Ba and K), indicating that fluids may subtly influence fO₂ duringmelting. However, for the most part, the average V/Sc-inferredfO₂s of arc basalts, MORB and peridotites are remarkably similar(–1·25 to +0·5 log units from the FMQ buffer)and disagree with the observation that the barometric fO₂s ofarc lavas are several orders of magnitude higher. These observationssuggest that the upper part of the Earth's mantle may be stronglybuffered in terms of fO₂. The higher barometric fO₂s of arclavas and some arc-related xenoliths may be due respectivelyto magmatic differentiation processes and to exposure to large,time-integrated fluid fluxes incurred during the long-term stabilityof the lithospheric mantle. KEY WORDS: vanadium; scandium; oxygen fugacity; mantle; arcs  相似文献   

凯氏蒸馏法和元素分析仪法测定沉积物中全氮含量的异同及其意义   总被引：2，自引：0，他引：2  

江伟  李心清  蒋倩  黄代宽  程红光 《地球化学》2006,35(3):319-324

氮循环是生物地球化学研究领域中最重要的课题之一,全氮含量的测定是农业、生物和环境等多领域研究中的常规测试项目。凯氏蒸馏法和元素分析仪法作为常规方法通用于上述领域的全氮含量测定,但两种方法在实际应用中的差异却常被忽视。通过对中国北方某盐湖沉积物序列近百个样品的全氮含量分析,对两种方法测定结果的异同进行了对比研究。凯氏蒸馏法的分析精密度高于元素分析仪法(前者标准偏差为0.007,后者为0.024),但在样品硝态和亚硝态氮的含量较高时,凯氏蒸馏法所测结果显著低于元素分析仪法的测定结果,此时选择元素分析仪法进行全氮含量的测定更为可靠和准确;对硝态和亚硝态氮含量极低的样品,两种方法的测定结果无显著差异。研究表明,选择全氮含量的测定方法,必须对所测样品的无机氮含量有初步的了解。对于中国北方的多数盐湖和地表环境样品,由于其无机氮的含量较高,选择凯氏蒸馏法进行全氮含量的测定是不适当的。尽管如此,对所研究的湖泊沉积物剖面而言,两种方法的对比却可以提供有价值的气候和环境演变信息。随着沉积物剖面的由深到浅,两种方法的测定结果由一致变化到存在显著差异,表明了湖泊水体从早期的淡水向今天的盐湖演化的过程。因此,凯氏蒸馏法和元素分析仪法测定结果的差异可以作为一种独立的地球化学气候代用指标。  相似文献   

“数字台湾”与中央山脉保育轴之划设、经营和管理     

郭琼莹李天任  伍肇雄 《地球信息科学学报》2002,4(3):8-16

本研究系应用数字地球系统理论于中央山脉保育轴经营管理机制建置 ,并依 IUCN之保育区划设标准 ,作为未来研订中央山脉保育计划之分区准则与数字台湾系统建立之发展模式。数字台湾之观念乃源于数字地球突破传统信息空间、政策经营之多向度信息整合 ,同时考虑克服科技应用与时间效益以及决策兼蓄解决传统资源管理在空间地理与生态艺术上之综合性问题。  相似文献   

PROBABLE MAXIMUM FLOOD FOR DAM SAFETY ASSESSMENT     

C.F.LEE 《国际泥沙研究》1996,(2)

ＰＲＯＢＡＢＬＥＭＡＸＩＭＵＭＦＬＯＯＤＦＯＲＤＡＭＳＡＦＥＴＹＡＳＳＥＳＳＭＥＮＴＣ．Ｆ．ＬＥＥ（Ｆｏｒｍｅｒｌｙ，ＭａｎａｇｅｒｏｆＧｅｏｔｅｃｈｎｉｃａｌａｎｄＨｙｄｒａｕｌｉｃＥｎｇｉｎｅｅｒｉｎｇＤｅｐａｒｔｍｅｎｔ；ＭａｎａｇｅｒｏｆＣｉ...  相似文献   

Melt Enrichment of Shallow Depleted Mantle: a Detailed Petrological, Trace Element and Isotopic Study of Mantle-Derived Xenoliths and Megacrysts from the Cameroon Line   总被引：4，自引：4，他引：4  

LEE  DER-CHUEN; HALLIDAY  ALEX N.; DAVIES  GARETH R.; ESSENE  ERIC J.; FITTON  J. GODFREY; TEMDJIM  ROBERT 《Journal of Petrology》1996,37(2):415-441

Major element, trace element and Sr–Nd–Pb isotopiccompositions of ultramafic xenoliths and megacrysts from thecontinental Cameroon line provide evidence for metasomatismof the upper most lithospheric mantle by enriched melts duringthe Mesozoic The megacrysts probably crystallized within thelower continental crust from melts similar to the host magmas.All the xenoliths originated as depleted residues after theextraction of basaltic melts, but some indicate evidence ofinteraction with enriched partial melts before entrainment.The U–Pb isotopic data on garnet are consistent with coolingthrough >900C at >300 Ma. The Sm–Nd isotope systematicsin constituent phases appear to have been in equilibrium ona xenolith scale at the time of entrainment, indicating derivationfrom mantle that remained at temperatures >600C until eruption.Spinel therzolies that show simple light rare earth element(LREE) depletions are characterized by isotopic compositionsthat are comparable with, but slightly more depleted than AtlanticN-MORB, suggesting that the unmetasomatized sub-continentallithosphere of the Cameroon line may be isotopically similarto that of sub-oceanic lithosphere. The Nd-depleted mantle modelages of these xenoliths are consistent with late Proterozoicdepletion, similar in age to much of the overlying continentalcrust. In contrast, samples that have LREE-enriched clinopyr-oxenes(La/Yb =4.7–9.4) contain trace amounts of amphibole, areenriched in U and have more radiogenic Pb and Sr. These xenolithsyield U–Pb and Sm–Nd model ages consistent withMesozoic enrichment, in agreement with the age of enrichmentof the source regions of the basalts, as deduced from Pb isotopiccompositions. Clinopyroxenes record three orders of magnitudeenrichment in U and LREE accompanied by progressive K depletionassociated with the growth of trace amphibole, with K/U ratiosthat range from 12000 to 1. The ratios of the trace elementsthought to have similar bulk D in mantle melting, Ce/Pb, Ba/Rband Nd/Sr ratios, display regional variations related to thetime integrated history of enrichments indicated by Nd isotopiccompositions. Mass balance calculations suggest that the meltsresponsible for the most recent enrichment of the lithospherehad higher La/Yb and U/Pb than Cameroon line host magmas, andwere probably the product of small degrees of partial meltingassociated with the earliest stages of the breakup of Pangea. KEY WORDS: Cameroon line; mantle xenoliths; megacrysts; REE; isotopic composition; trace element  相似文献