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131.
Late Glacial and Neoglacial (Little Ice Age) deposits on the Humboldt Massif were analyzed for relative-age dating parameters, including geomorphic and weathering characteristics, geochemical and soil properties. The soil chronosequence, formed in chemically uniform parent materials, provides an important database to study soil evolution in a tropical alpine environment. Extractable and total Fe and Al concentrations, examined to assess their use in relative-age determination, and as paleoenvironmental indicators, provide an important measure of the accumulation and downward profile movement over time of organically-bound Al, ferrihydrite and other crystalline forms (hematite and goethite) of extractable Fe. Ferrihydrite is particularly useful in determining former perched water levels in soils with relation to paleoclimate. The ratios of most Fe extracts are time dependent. The Fed/Fet ratio, within statistical limits, shows a slow increase from LIA (Little Ice Age) to Late Glacial soils, which closely correlates with other alpine soil studies in the middle latitudes and other tropical alpine locales. Values of Ald (dithionite) and Alo (oxalate extractable) generally do not correlate with time; however, Alp (pyrophosphate extractable) measured against Alt (total) provides insight on the downward translocation over time of organically-bound Al. Low leaching rates in this chronosequence are further supported by clay mineralogy trends and the geochemical data. 相似文献
132.
133.
Impact of fertilizer phosphorus application on phosphorus release kinetics in some calcareous soils 总被引:1,自引:0,他引:1
Phosphate reactions and retention in the soil are of paramount importance from the perspective of plant nutrition and fertilizer
use efficiency. The objective of this work was to study the kinetics of phosphorus (P) desorption in different soils of Hamadan
in fertilized and unfertilized soils. Soils were fertilized with 200 mg P kg−1. Fertilized and unfertilized soils were incubated at 25 ± 1°C for 6 months. After that, release of P was studied by successive
extraction with 0.5 M NaHCO3 over a period of 1,752 h. The results showed that phosphorus desorption from the fertilized and unfertilized soils began
with a fast initial reaction, followed by a slow secondary reaction. The amount of P released after 1,752 h in fertilized
and unfertilized soils ranged from 457 to 762.4 and 309.6 to 586.7 mg kg−1, respectively. The kinetics of cumulative P release was evaluated using the five kinetic equations. Phosphorus desorption
kinetics were best described by parabolic diffusion law, first order, and power function equations. Rate constants of these
equations were higher in fertilized than unfertilized soils. Results from this study indicate that release rate of P plays
a significant role in supplying available P and released P in runoff. 相似文献
134.
135.
S. Tadisetty K. Matsui H. Shimada R. N. Gupta 《Rock Mechanics and Rock Engineering》2006,39(4):383-393
Summary. Discontinuous manual observations and irregular caving characteristics of roof rocks often lead to improper decisions resulting
in accidents and production loss. Hence, systematic monitoring of the hanging roof behind the chock shields is necessary for
safe and productive mining operations. A real-time application was successfully implemented in an Indian mine for forecasting
of hanging roof behaviour to enhance safety and productivity. This paper reports the functioning of real-time TWAP (time weighted
average pressure) analysis in the forecasting of hanging roof behaviour in real time. 相似文献
136.
Naidu L.S. G. Rao V.V.S. T. Rao G. Mahesh J. Padalu G. Sarma V.S. Prasad P.R. Rao S.M. R. Rao B.M. 《Arabian Journal of Geosciences》2013,6(10):3709-3724
The Central Godavari delta is located along the Bay of Bengal Coast, Andhra Pradesh, India, and is drained by Pikaleru, Kunavaram and Vasalatippa drains. There is no groundwater pumping for agriculture as wells as for domestic purpose due to the brackish nature of the groundwater at shallow depths. The groundwater table depths vary from 0.8 to 3.4 m and in the Ravva Onshore wells, 4.5 to 13.3 m. Electrical Resistivity Tomography (ERT) surveys were carried out at several locations in the delta to delineate the aquifer geometry and to identify saline water aquifer zones. Groundwater samples collected and analyzed for major ions for assessing the saline water intrusion and to identify the salinity origin in the delta region. The results derived from ERT indicated low resistivity values in the area, which can be attributed to the existence of thick marine clays from ground surface to 12–15 m below ground level near the coast and high resistivity values are due to the presence of coarse sand with freshwater away from the coast. The resistivity values similar to saline water <0.01 Ω m is attributed to the mixing of the saline water along surface water drains. In the Ravva Onshore Terminal low resistivity values indicated up coning of saline water and mixing of saline water from Pikaleru drain. The SO 4 ?2 /Cl?and Na+2/Cl?ratios did not indicate saline water intrusion and the salinity is due to marine palaeosalinity, dilution of marine clays and dissolution of evaporites. 相似文献
137.
Site response studies in Agartala Urban agglomeration 总被引:1,自引:0,他引:1
A systematic investigation using digital microearthquake recorders with short period SS-1 seismometers, covering 76 sites
in and around Agartala city, has been carried out for site response (SR) studies in the area. In the northern part of the
area, SR varies from 1.15 to 1.85 corresponding to peak frequency 0.76 to 0.93 Hz where soil is mostly semi-consolidated and
stiffer than recent Quaternary deposits (Haora River formation). In the southern part of the area, SR varies from 1.12 to
2.42 corresponding to peak frequency from 0.71 to 0.85 Hz within the Dupitila formation (early Quaternary). It is observed
that estimated SR from H/V increases from edges to middle of the Haora River valley and impedance contrast fallows the similar
trend. This reflects that site response by H/V is influenced by impedance contrast, whereas computed amplification from 1-D
model shows opposite trend. The maximum amplification at fundamental frequency of resonance, 1.04 Hz estimated from H/V by
near to BH-7, is 2.5 times greater than the impedance contrast/ratio derived from 1-D model for same location. Relationship
between resonance frequency and depth was obtained by applying quarter wavelength and Bard (2000) methodologies, which shows linearity, whereas H/V shows its nonlinearity characteristic in soil across the valley part of
Haora River. Shear wave velocities, and subsequently, SPT index and factor of safety (by cyclic stress approach) were estimated
from geotechnical parameters. Vs30 and site response data were used in this study for getting a first hand information about
soil stiffness condition in the area. The estimation of SPT index and factor of safety could be a useful tool for delineating
liquefied and none liquefied zones at various depth levels, especially where water table exists at a very shallow level. The
expected liquefiable zone was observed at depths varying from 6–25 m beneath the soil bearing zones where percentage of fines
is estimated to be more than 35% for the area. This knowledge about subsurface soil characteristics will be useful for the
civil engineers/city planners, which can be taken into account at the time of constructing earthquake-resistant structures
in the area. 相似文献
138.
Tim R. Orr 《Bulletin of Volcanology》2011,73(3):335-346
Shatter rings are circular to elliptical volcanic features, typically tens of meters in diameter, which form over active lava
tubes. They are typified by an upraised rim of blocky rubble and a central depression. Prior to this study, shatter rings
had not been observed forming, and, thus, were interpreted in many ways. This paper describes the process of formation for
shatter rings observed at Kīlauea Volcano during November 2005–July 2006. During this period, tilt data, time-lapse images,
and field observations showed that episodic tilt changes at the nearby Pu‘u ‘Ō‘ō cone, the shallow magmatic source reservoir,
were directly related to fluctuations in the level of lava in the active lava tube, with periods of deflation at Pu‘u ‘Ō‘ō
correlating with increases in the level of the lava stream surface. Increases in lava level are interpreted as increases in
lava flux, and were coincident with lava breakouts from shatter rings constructed over the lava tube. The repetitive behavior
of the lava flux changes, inferred from the nearly continuous tilt oscillations, suggests that shatter rings form from the
repeated rise and fall of a portion of a lava tube roof. The locations of shatter rings along the active lava tube suggest
that they form where there is an abrupt decrease in flow velocity through the tube, e.g., large increase in tube width, abrupt
decrease in tube slope, and (or) sudden change in tube direction. To conserve volume, this necessitates an abrupt increase
in lava stream depth and causes over-pressurization of the tube. More than a hundred shatter rings have been identified on
volcanoes on Hawai‘i and Maui, and dozens have been reported from basaltic lava fields in Iceland, Australia, Italy, Samoa,
and the mainland United States. A quick study of other basaltic lava fields worldwide, using freely available satellite imagery,
suggests that they might be even more common than previously thought. If so, this confirms that episodic fluctuation in lava
effusion rate is a relatively common process at basaltic volcanoes, and that the presence of shatter rings in prehistoric
lava flow fields can be used as evidence that such fluctuations have occurred. 相似文献
139.
140.