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101.
Lateral response of dams in semi-elliptical rigid canyons 总被引:2,自引:0,他引:2
An analytical closed-form solution is developed for the lateral response of earth and rockfill dams built in semi-elliptical canyons. The dam is idealized as a linearly hysteretic elastic body deforming only in shear, whereas the canyon is assumed to be rigid. The solution for the dam response is given in terms of prolate spheroidal radial and angular functions of the first kind and zero order. Results are presented for natural frequencies, modal displacement shapes, participation factors, and response to transient and steady-state harmonic base excitation for various dam length-to-height ratios. Comparisons are made of the effects of the length-to-height ratio and the canyon shape on the response of dams built in semi-elliptical and rectangular canyons. A subsequent study (Dakoulas, P. & Hsu, C.H., Response of earth dams in semi-elliptical flexible canyons to oblique SH waves, Report, Rice University, Houston, Texas, 1993) extends this model to a semi-elliptical canyon consisting of flexible elastic rock, subjected to obliquely incident harmonic SH waves. 相似文献
102.
Specially designed arrays of strong-motion seismographs near to the earthquake source are required for seismological and engineering studies of the generation and near-field properties of seismic waves. The first such large digital array, called SMART 1 (with radius 2 km and 37 accelerometers), to record substantial ground motion (up to 0·24g horizontal acceleration) became operational in late 1980 in a highly seismic region of Taiwan. During the first 6 months of operation, SMART 1 recorded nine earthquakes with magnitudes ranging from ML 3·8 to 6·9. Three were located directly below the array at focal depths of 59 to 76 km. The remaining six had shallow depths and epicentral distances from 7 to 193 km. Digital records from 27 three-component accelerographs were obtained from a magnitude 6·9 (ML) local earthquake on 29 January 1981. Representative measurements are described of seismic wave coherency and power spectrum as a function of wave number, frequency, azimuth of propagation and wave type. Acceleration waveforms varied significantly across the array for each event. On average, peak acceleration of horizontal components was about three times that of the vertical component. Relative spectral changes from earthquake to earthquake were large. 相似文献
103.
Selected by-products which are produced upon chlorination or ozonization of seawater were examined for their effect on eastern oyster (Crassostrea virginica) larvae. The compounds, bromate, bromoform, and chloroform, were studied at 0.05, 0.1, 1.0, and 10.0 mg/l. Repeated bioassays indicated that even at these low levels, all three substances produced some larval mortality. This preliminary study suggests that oxidation by-products formed during chlorination or ozonization of power plant cooling waters may have adverse effects upon the growth of marine invertebrates, such as C. virginica, during their delicate larval stages. 相似文献
104.
Abstract— We have made aluminum‐magnesium isotopic measurements on 4 melilite‐bearing calcium‐aluminum‐rich inclusions (CAIs), 1 plagioclase‐olivine inclusion (POI), and 2 ferromagnesian chondrules from the Ningqiang carbonaceous chondrite. All of the CAIs measured contain clear evidence for radiogenic 26Mg* from the decay of 26Al ( = 1.05 Ma). Although the low Al/Mg ratios of the melilites introduce large uncertainties, the inferred initial 26Al/27Al ratios for the CAIs are generally consistent with the value of 5 times 10?5. There is clear evidence of 26Al* in one POI and two chondrules, but with considerable uncertainties in the value of (26Al/27Al)0. The (26Al/27Al)0 ratios for the POI and the chondrules are 0.3–0.6 times 10?5, roughly an order of magnitude lower than the canonical value. Ningqiang shows very little evidence of metamorphism as a bulk object and the (26Al/27Al)0 ratios in its refractory inclusions and chondrules are consistent with those found in other unmetamorphosed chondrites of several different classes. Our observations and those of other workers support the view that 26Al was widely and approximately homogeneously distributed throughout the condensed matter of the solar system. The difference in (26Al/27Al)0 between CAIs and less refractory materials seems reasonably interpreted in terms of a ~2 million year delay between the formation of CAIs and the onset of formation of less refractory objects. The POI shows clear differences in 25Mg/24Mg between its constituent spinels and olivine, which confirms that they are partially reprocessed material from different sources that were rapidly quenched. 相似文献
105.
Great interest has recently been focused on dating and interpreting alluvial-fan surfaces. As a complement to the radiometric methods often used for surface-exposure dating, this paper illustrates a rapid method for correlating and dating fan surfaces using the cross-sectional shape of gullies incised into fan surfaces. The method applies a linear hillslope-diffusion model to invert for the diffusivity age, κt (m2), using an elevation profile or gradient (slope) profile. Gullies near the distal end of fan surfaces are assumed to form quickly following fan entrenchment. Scarps adjacent to these gullies provide a measure of age. The method is illustrated on fan surfaces with ages of approximately 10 ka to 1.2 Ma in the arid southwestern United States. Two areas of focus are Death Valley, California, and the Ajo Mountains piedmont, Arizona. Gully-profile morphology is measured in two ways: by photometrically derived gradient (slope) profiles and by ground-surveyed elevation profiles. The κt values determined using ground-surveyed profiles are more consistent than those determined using photo-derived κt values. However, the mean κt values of both methods are comparable. The photometric method provides an efficient way to quantitatively and objectively correlate and relatively-date alluvial-fan surfaces. The κt values for each surface are determined to approximately 30–50% accuracy. 相似文献
106.
Coastal Gravity Anomalies from Retracked Geosat/GM Altimetry: Improvement, Limitation and the Role of Airborne Gravity Data 总被引:6,自引:0,他引:6
Cheinway Hwang Jinyun Guo Xiaoli Deng Hsin-Ying Hsu Yuting Liu 《Journal of Geodesy》2006,80(4):204-216
We process geophysical and waveform data records of the Geosat/GM (geodetic mission) satellite altimeter mission for waveform retracking and applications. An improved threshold retracker is developed. The performances of the Beta-5, threshold and improved threshold retrackers are assessed over waters around Taiwan. The improved threshold retracker outperforms the other two. The improvement in the accuracy of sea surface height (SSH) is investigated according to marine zone and the distance of waters to the shore. The improvement rate increases closer to the land, with the largest improvement rate of about 20% in waters within 10 km of the shore. Over waters around islands and coasts, there are still retracked SSHs with large errors. Least-squares collocation is used to compute gravity anomalies from the Geosat/GM altimeter data. Use of retracked SSHs improves the accuracy of gravity anomalies by about 11%. Adding airborne gravity data further improves the accuracy, especially in the immediate vicinity of the coasts. Tide model errors over coastal waters remain a problem in altimetry applications, even if the waveforms are properly retracked. 相似文献
107.
In this contribution we introduce the concept of multiresolution analysis (MRA) and give an explanation of the relationship
between MRA and orthonormal wavelet basis. The construction of the orthonormal B-spline wavelet bases is described in detail.
We extend the B-splines to `non-integral order' cases and thus obtain a new family of orthonormal wavelet bases for the space
L
2(R). Some good properties of the new wavelets are demonstrated. The new wavelet family gives satisfactory performances in our
research projects including seismic signal compression and gravity tide data processing.
Received: 19 July 1996 / Accepted: 17 November 1997 相似文献
108.
Shiang-Kueen Hsu 《Hydrogeology Journal》1998,6(3):405-415
In Taiwan, rapid economic growth, rising standards of living, and an altered societal structure have in recent years put
severe demands on water supplies. Because of its stable quantity and quality, groundwater has long been a reliable source
of water for domestic, agricultural, and industrial users, but the establishment of a management program that integrates groundwater
and surface-water use has been hampered by the lack of groundwater data. In 1992, the Department of Water Resources (DWR)
initiated a program entitled "Groundwater Monitoring Network Plan in Taiwan." Under this program, basic groundwater data,
including water-level and water-quality data, are being collected, and a reliable database is being established for the purpose
of managing total water resources. This paper introduces the goals, implementation stages, and scope of that plan. The plan
calls for constructing 517 hydrogeologic survey stations and 990 groundwater monitoring wells within 17 years. Under this
program, water-level fluctuations are continuously monitored, whereas water-quality samples are taken for analysis only at
the initial drilling stage and, subsequently, at the time when a monitoring well is being serviced. In 1996, the DWR and the
Water Resources Planning Commission were merged to form today's Water Resources Bureau.
Received, July 1997 · Revised, February 1998 · Accepted, January 1998 相似文献
109.
110.
模拟大地水准面应用于GPS水准内插的研究 总被引:2,自引:0,他引:2
采用移去-恢复技术和多面函数法对已知GPS水准数据进行了内插处理。试验结果表明.利用实际地球物理资料得到的模拟大地水准面精度最高。 相似文献