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171.
Two-Dimensional Mathematical Model of Tidal Current and Sediment for Oujiang Estuary and Wenzhou Bay 总被引:3,自引:0,他引:3
A 2-D mathematical model of tidal current and sediment has been developed for the Oujiang Estuary and the Wenzhou Bay. This model accomodates complicated features including multiple islands, existence of turbidity, and significant differ-ence in size distribution of bed material. The governing equations for non-uniform suspended load and bed load transport are presented in a boundary-fitted orthogonal curvilinear coordinate system. The numerical solution procedures along with their initial conditions, boundary conditions, and movable boundary technique are presented. Strategies for computation of the critical condition of deposition or erosion, sediment transport capacity, non-uniform bed load discharge, etc. are suggested. The model verification computation shows that, the tidal levels computed from the model are in good agreement with the field data at the 18 tidal gauge stations. The computed velocities and flow directions also agree well with the values measured along the totally 52 synchronously ob 相似文献
172.
综合分析兴文MS5.7地震672个余震的精定位结果、应力背景和深部背景认为,兴文MS5.7地震是由北东-南西向隐伏断层所引起。北西-南东向的水平最大主应力持续挤压引发破裂,形成MS5.7主震;其他3次地震与兴文MS5.7地震呈北东向线性排列,结合震源机制解和应力方向分析认为,其他3次地震也与该隐伏断层有关。 相似文献
173.
A double index (DI), which is made up of two sub-indices, is proposed to describe the spatial patterns of the Kuroshio intrusion and mesoscale eddies west to the Luzon Strait, based on satellite altimeter data. The area-integrated negative and positive geostrophic vorticities are defined as the Kuroshio warm eddy index (KWI) and the Kuroshio cold eddy index (KCI), respectively. Three typical spatial patterns are identified by the DI: the Kuroshio warm eddy path (KWEP), the Kuroshio cold eddy path (KCEP), and the leaking path. The primary features of the DI and three patterns are further investigated and compared with previous indices. The effects of the integrated area and the algorithm of the integration are investigated in detail. In general, the DI can overcome the problem of previously used indices in which the positive and negative geostrophic vorticities cancel each other out. Thus, the proportions of missing and misjudged events are greatly reduced using the DI. The DI, as compared with previously used indices, can better distinguish the paths of the Kuroshio intrusion and can be used for further research. 相似文献
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黑潮延伸体海表温度锋位置的变化特征 总被引:2,自引:1,他引:1
High spatial resolution sea surface temperature(SST) data from 1993 to 2013 are used to detect the position of the Kuroshio Extension sea surface temperature front(KEF) from 141°E to 158°E,and the seasonal,monthly and interannual-to-decadal variations of the KEF position are investigated.The latitudinal position of the KEF varies with longitudes:the westernmost part of the KEF from 141°E to 144°E is relatively stable,whereas the easternmost part from 153°E to 158°E exhibits the largest amplitude of its north-south displacement.In the light of the magnitudes of the standard deviations at longitudes,then the KEF is divided into three sections:western part of the KEF(KEFw,141°–144°E),central part of the KEF(KEFc,144°–153°E) and eastern part of the KEF(KEFe,153°–158°E).Further analysis reveals that the KEFw position is dominated by the decadal variability,while the KEFc and KEFe positions change significantly both on interannual and decadal time scales.In addition,the KEFw position is well correlated with the KEF path length.The possible mode leading to the decadal oscillation of the KEFw is further discussed.The KEFw position exhibits significant connections with the Pacific decadal oscillation(PDO) index and the north Pacific gyre oscillation(NPGO) index with a time lag of 40 and 33 months,respectively. 相似文献
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178.
有机相研究及其在盆地分析中的应用 总被引:14,自引:0,他引:14
有机相是具有一定丰度和特定成因类型的有机质的地层单元,决定有机相类型的最重要参数是干酪根的成因类型。为了反映沉积盆地中有机相的时空分布,我们提出了有机相组合和盆地有机充填序列等新概念。有机相及有机相层序、有机充填序列和有机相组合不仅是预测和在三维空间确定生油岩的分布、预测主力生油岩的排烃期和排出产物的组成的有效工具,而且可以弥补以骨架砂岩体为主要研究对象的沉积学分析的不足,在确定层序界线或不整合面的位且、研究盆地的构造沉降和沉积充填史等方面发挥重要作用。 相似文献
179.
云南抚仙湖水体营养元素分布及其对人为扰动的响应 总被引:4,自引:0,他引:4
本文分析了云南抚仙湖水体营养元素和溶解氧的分布特征,并结合大洋协会在湖区进行的多金属结核采矿系统试验,探讨了采矿系统在湖底行走而导致的人为扰动对湖区营养元素的影响。研究表明,湖区水体中的营养元素存在着明显的季节性变化,且主要受湖区气候水文条件的影响;采矿系统行走时所扰动的沉积物对水体中的营养元素,尤其是近底层水体的营养元素分布,影响明显,这主要是由于再悬浮的沉积物将原先吸附在沉积物上的营养元素再次释放到水体中而导致的,因此,在评价人类湖底采矿试验活动对湖区环境的影响时还应关注湖底沉积物对水环境的影响。 相似文献
180.
A case study on the cyclonic eddy generated by the tropical cyclone looping over the northern South China Sea (NSCS) is presented, using TOPEX/POSEIDON altimeter data and AVHRR sea surface temperature (SST) data.Three cases relating to the tropical cyclone events (Typhoon Kai-Tak in July 2000, Tropical Storm Russ in June 1994and Tropical Storm Maria in August-September 2000) over the NSCS have been analyzed. For each looping tropical cyclone case, the cyclonic eddy with an obvious sea level depression appears in the sea area where the tropical cyclone takes a loop form, and lasts for about 2 weeks with a slight variation in location. The cold core with the SST difference greater than 2 ℃ against its surrounding areas is also observed by the satellite-derived SST data. 相似文献