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691.
Phosphorus Sorption Dynamics of Hawaii’s Coastal Wetlands 总被引:2,自引:0,他引:2
While phosphorus (P) sorption has been studied in Hawaii’s terrestrial soils, P sorption dynamics have yet to be investigated
in coastal wetlands. In other coastal zones, wetlands have been shown to sorb P and act as P sinks at the land–sea interface.
Thus, the objectives of this study were to examine variance in the P sorption index (PSI) within wetlands along hydrologic
gradients and among wetlands of different types and to identify soil properties that best explain variability in the PSI.
Forty wetlands on five islands were sampled and P sorption and related properties were measured. Phosphorus sorption index
values ranged from −16.4–1,732.5. Hydrologic zone (within sites) and surface water salinity (among sites) accounted for significant
proportions of the variance in the PSI. While texture, pH, and carbon content were found to be important predictors of PSI,
the highest correlations were found for oxalate-extractable iron. 相似文献
692.
693.
Pakama Queenscious Siyongwana 《GeoJournal》2009,74(4):293-310
The demise of South African Apartheid Planning in 1994 and subsequent lost of Umtata’s capital status when the Transkei was
subsumed into the new Eastern Cape Province resulted in the major political transformation of the Transkei state. Central
to the post-apartheid transformation was restructuring of Transkei bureaucracy which at the time of South Africa’s independence
in 1994 displayed abnormalities. This paper documents the restructuring of the Transkei bureaucracy focusing on Umtata since
1994. The study has brought to the forefront the following facts: Firstly, that at the time of the Transkei merger into South
Africa, employment in the government was ‘booming’ and to greater extent it was affected by Umtata’s role—being the capital
city of the pseudo-Transkei state. Secondly, the post 1994-political transformation of the Transkei Bantustan impacted negatively
on Umtata’s employment notably the civil service sector by ‘squeezing’ it during the early years of democracy (1994–2000).
Thirdly, since 2001, with Umtata serving as the major urban centre of both King Sabata Local Municipality and OR Tambo District
Municipality, employment in the civil service and municipality has been revitalized. 相似文献
694.
Transparent exopolymer particle (TEP) distributions were examined in North Carolina’s Neuse River Estuary (NRE) over a 1-year
period, and experiments were conducted to examine controls upon TEP formation. TEP-carbon averaged 16% of the total organic
carbon pool in the NRE. From May to early August 2007, TEP ranged from 805 to 1,801 μg xanthan gum (XG) L−1. A large phytoplankton bloom peaked in early August and then subsequently declined. Within 2 weeks of the bloom’s peak, TEP
concentrations increased to >3,500 μg XG L−1 and remained elevated through mid-December. Decreasing water temperatures and enhanced retention due to drought conditions
in Fall 2007 likely aided in the persistence of TEP concentrations during this timeframe. Thereafter, TEP decreased coincident
with increased river flow and flushing of the estuary that began in January 2008, and TEP remained low (ranging from 991 to
1,712 μg XG L−1) until the end of April 2008. TEP was positively correlated with salinity, suggesting that cation availability (which co-varies
with salinity and stabilizes the structural integrity of TEP) may play a role in estuarine TEP formation. In two cation addition
experiments using water from the mesohaline region, TEP concentrations tended to be higher in treatments with vs. without
cations added. Statistically significant relationships were also found between in situ TEP concentrations and pH, mixing,
and temperature, suggesting that a complex suite of environmental parameters affect TEP formation and its distribution in
estuaries. 相似文献
695.
Mineralogy and geochemistry of banded iron formation and iron ores from eastern India with implications on their genesis 总被引:1,自引:0,他引:1
The geological complexities of banded iron formation (BIF) and associated iron ores of Jilling-Langalata iron ore deposits,
Singhbhum-North Orissa Craton, belonging to Iron Ore Group (IOG) eastern India have been studied in detail along with the
geochemical evaluation of different iron ores. The geochemical and mineralogical characterization suggests that the massive,
hard laminated, soft laminated ore and blue dust had a genetic lineage from BIFs aided with certain input from hydrothermal
activity. The PAAS normalized REE pattern of Jilling BIF striking positive Eu anomaly, resembling those of modern hydrothermal
solutions from mid-oceanic ridge (MOR). Major part of the iron could have been added to the bottom sea water by hydrothermal
solutions derived from hydrothermally active anoxic marine environments. The ubiquitous presence of intercalated tuffaceous
shales indicates the volcanic signature in BIF.
Mineralogical studies reveal that magnetite was the principal iron oxide mineral, whose depositional history is preserved
in BHJ, where it remains in the form of martite and the platy hematite is mainly the product of martite. The different types
of iron ores are intricately related with the BHJ. Removal of silica from BIF and successive precipitation of iron by hydrothermal
fluids of possible meteoric origin resulted in the formation of martite-goethite ore. The hard laminated ore has been formed
in the second phase of supergene processes, where the deep burial upgrades the hydrous iron oxides to hematite. The massive
ore is syngenetic in origin with BHJ. Soft laminated ores and biscuity ores were formed where further precipitation of iron
was partial or absent. 相似文献
696.
Long records of monthly salinity observations along the axis of Chesapeake Bay, Delaware Bay, and Long Island Sound are used
to test a simple advection–dispersion model of the salt distribution in linearly tapered estuaries developed in a previous
paper. We subdivide each estuary into three to five segments, each with linear taper allowing a distributed input of fresh
water, and evaluate the dispersion in each segment. While Delaware Bay has weak dispersion and a classical sigmoidal salinity
structure, Long Island Sound and Chesapeake Bay are more dispersive and have relatively small gradients in the central stretches.
Long Island Sound is distinguished by having a net volume and salt flux out of its low-salinity end resulting in a smaller
range of salinity and increasing axial gradients at its head rather than the usual asymptotic approach to zero salinity. Estimates
of residence times based on model transport coefficients show that Long Island Sound has the most rapid response to fresh-water
flux variations. It also has the largest amplitude cycle in river discharge fluctuation. In combination, these cause the large
seasonal variation in the salinity structure relative to interannual variability in Long Island Sound as compared with Chesapeake
Bay and Delaware Bay. 相似文献
697.
On 19 April 2005, an oil spill occurred in southeastern Louisiana’s Barataria Bay estuary. We used a drop sampler to characterize
the marsh-edge nekton community. Thirty-six locations were sampled in pre- and post-spill time frames from March through May
2005. Before–after control–impact (BACI) analyses of the total number of individuals (fishes + decapod crustaceans), total
fishes, and sensitive species found significant interactions between the temporal (before/after) and spatial (control/impact)
treatments and indicated an effect of the oil spill. Nonparametric analyses detected varied faunal assemblages across temporal
treatments, but were similar in species composition among spatial treatments. While the BACI analyses showed event effects,
differences were not strongly detected in nonparametric analyses of community structure. Fish are mobile and left the spill
area after the disturbance, whereas the less mobile but more numerous benthic decapod crustaceans remained. The overall community
structure appears to be robust and quickly recovered from the localized spill event. 相似文献
698.
The occurrence and development of riparian forests, which were mainly dominated by mesophytes species related closely with
surface water. Since there was no water discharged to the lower reaches of Tarim River in the past three decade years, the
riparian forests degrade severely. The groundwater table, the saline content of the groundwater, as well as the content of
free proline, soluble sugars, plant endogenous hormones (abscisic acid (ABA), and cytokinins (CTK)) of the leaves and relative
rates of sap flow of the Populus euphratica Oliv. (arbor species), Tamarix ramosissima Ldb. (bush species), and Apocynum venetum L. (herb species) were monitored and analyzed at the lower reaches of the Tarim River in the study area where five positions
on a transect were fixed at 100 m intervals along a sampling direction from riverbank to the sand dunes before and after water
release. The physiological responses and acclimation strategies of three species to variations in water and salinity stress
were discussed. It was found that A. venetum population recovered to groundwater table ranging from −1.73 to −3.56 m, and when exposed to saline content of the groundwater
ranging from 36.59 to 93.48 m mol/L; P. euphratica appeared to be more sensitive to the elevation of groundwater table than the A. venetum and T. ramosissima at groundwater table ranging from −5.08 to −5.80 m, and when exposed to saline content of the groundwater ranging from 42.17
to 49.55 m mol/L. T. ramosissima tended to be the best candidate species for reclamation in this hyper-arid area because it responded to groundwater table
ranging from −1.73 to −7.05 m, and when exposed to saline content of the groundwater ranging from 36.59 to 93.48 m mol/L.
These results explained the distribution patterns of desert vegetation in the lower reaches of the Tarim River. Understanding
the relationships among ecological factors variables, physiological response and acclimation strategies of plant individuals
could provide guidance to sustainable management, reclamation and development of this and similar regions. 相似文献
699.
Theodore D. Kanellopoulos Michael O. Angelidis Dimitrios Georgopoulos Aristomenis P. Karageorgis 《Environmental Geology》2009,57(8):1729-1738
Evros River is the most important river flowing into the North Aegean Sea (eastern Mediterranean) in terms of freshwater discharge,
and the second largest one of Eastern Europe after the Danube River. Salinity and temperature measurements, together with
suspended particulate matter concentrations were obtained in various depths at 14 stations in the adjacent Alexandroupolis
Gulf during four seasons (June 1998, September 1998, February 1999 and March 2000) in order to investigate the particle dynamics
and distributions in the northern Aegean Sea. Analysis of the collected data, together with particle observations under the
scanning electron microscope and study of satellite images showed that, under certain circumstances driven by the hydrological
and wind regime of the area, the Evros River particulate matter, with the associated pollutants, can be transferred far away
from the estuary and implicitly comprise a hazardous factor for the environmental status of the northern Aegean Sea. This
fact, combined with the future construction of the Burgas-Alexandroupolis pipeline, may cause a negative impact on the studied
natural ecosystem. 相似文献
700.
The Valhalla uranium deposit, located 40 km north of Mount Isa, Queensland, Australia, is an albitite-hosted, Mesoproterozoic
U deposit similar to albitite-hosted uranium deposits in the Ukraine, Sweden, Brazil and Guyana. Uranium mineralisation is
hosted by a thick package of interbedded fine-grained sandstones, arkoses and gritty siltstones that are bound by metabasalts
belonging to the ca. 1,780 Ma Eastern Creek Volcanics in the Western Succession of the Mount Isa basin. Alteration associated
with U mineralisation can be divided into an early, main and late stage. The early stage is dominated by laminated and intensely
altered rock comprising albite, reibeckite, calcite, (titano)magnetite ± brannerite. The main stage of mineralisation is dominated
by brecciated and intensely altered rocks that comprise laminated and intensely altered rock cemented by brannerite, apatite,
(uranoan)-zircon, uraninite, anatase, albite, reibeckite, calcite and hematite. The late stage of mineralisation comprises
uraninite, red hematite, dolomite, calcite, chlorite, quartz and Pb-, Fe-, Cu-sulfides. Brannerite has U–Pb and Pb–Pb ages
that indicate formation between 1,555 and 1,510 Ma, with significant Pb loss evident at ca. 1,200 Ma, coincident with the
assemblage of Rodinia. The oldest ages of the brannerite overlap with 40Ar/39Ar ages of 1,533 ± 9 Ma and 1,551 ± 7 Ma from early and main-stage reibeckite and are interpreted to represent the timing
of formation of the deposit. These ages coincide with the timing of peak metamorphism in the Mount Isa area during the Isan
Orogeny. Lithogeochemical assessment of whole rock data that includes mineralised and unmineralised samples from the greater
Mount Isa district reveals that mineralisation involved the removal of K, Ba and Si and the addition of Na, Ca, U, V, Zr,
P, Sr, F and Y. U/Th ratios indicate that the ore-forming fluid was oxidised, whereas the crystal chemistry of apatite and
reibeckite within the ore zone suggests that F− and were important ore-transporting complexes. δ18O values of co-existing calcite and reibeckite indicate that mineralisation occurred between 340 and 380°C and involved a
fluid having δ18Ofluid values between 6.5 and 8.6‰. Reibeckite δD values reveal that the ore fluid had a δDfluid value between −98 and −54‰. The mineral assemblages associated with early and main stages of alteration, plus δ18Ofluid and δDfluid values, and timing of the U mineralisation are all very similar to those associated with Na–Ca alteration in the Eastern
Succession of the Mount Isa basin, where a magmatic fluid is favoured for this style of alteration. However, isotopic data
from Valhalla is also consistent with that from the nearby Mount Isa Cu deposit where a basinal brine is proposed for the
transport of metals to the deposit. Based on the evidence to hand, the source fluids could have been derived from either or
both the metasediments that underlie the Eastern Creek Volcanics or magmatism that is manifest in the Mount Isa area as small
pegmatite dykes that intruded during the Isan Orogeny. 相似文献