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61.
62.
Sushmitha Baskar R. Baskar Natuschka Lee A. Kaushik P. K. Theophilus 《Environmental Geology》2008,56(2):237-243
The Borra caves, Vishakapatnam, India, can be described as a speleothem cave with significant amounts of unexplored microbial
mats in spring waters. Here, we present the first observations and hypotheses on the possible impact of the microorganisms
in these mats on the cave formation, focusing on their role on iron mineral precipitation. The spring waters (pH neutral 7.5–7.7)
contained dissolved metals like iron and the organic mat sludge (pH 7.0–7.3) had a TOC content of approximately 5.4 wt%. Geochemically,
the spring waters deep below the microbial mats contained Fe 369 ppb, Sr 198 ppb; and the organic mat sludge contained Mg
9 ppm, Fe 427 ppb, Zn 149 ppb, Sr 190 ppb. XRD observations displayed Fe minerals (dominantly hematite), minor amounts of
zinc gallium sulfide and nitrofuryl compounds. At least four groups of bacteria identified by direct microscopy and SEM-EDX
on the basis of morphology could be observed in all samples: Leptothrix-like organisms, entombed bacterial mineral sheaths, a few stalks of Gallionella-like organisms and some additional bacteria that could not be further identified. Leptothrix-like organisms contained 43.22–60.08 wt % Fe and the mineral precipitated near and around these bacteria (in the actual unaltered
samples on site) contained 30.76–45.22 wt% Fe as identified and quantified by SEM-EDX. This study indicates that the precipitation
of these iron-rich mats in the spring waters could be linked to the presence of abundant active communities of iron precipitating
bacteria at Borra caves, Vishakapatanam. 相似文献
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Sunghan Kim Kozo Takahashi Boo-Keun Khim Yoshihiro Kanematsu Hirofumi Asahi Ana Christina Ravelo 《Quaternary Research》2014
Biogenic opal content and mass accumulation rate (MAR) at IODP Expedition 323 Site U1343 were found to fluctuate consistently, generally being high under warm conditions and low under cold conditions during the last 2.4 Ma. Continuous wavelet transform analysis of the normalized biogenic opal content indicates that export production in the Bering Sea varied predominantly at 41-ka periodicity before 1.25 Ma, and shifted to 100-ka periodicity at the onset of the Mid-Pleistocene Transition (MPT; 1.25–0.7 Ma). The 100-ka cycles dominated until the Holocene. Export production in the Bering Sea decreased markedly in the Bering Sea two times during the MPT: the first occurred at the beginning of the MPT (1.25 Ma) and the second in the middle of the MPT (0.9 Ma). These decreases coincided with both increases in the relative abundance of sea-ice diatoms and decreases in the warm-water diatom species Neodenticula seminae, indicating that reductions in export production in the Bering Sea during the MPT were associated with climate cooling. Decreases in export production in the Bering Sea during the MPT were most likely associated with the increased influence of polar/Arctic domains on the high-latitude North Pacific. 相似文献
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In this paper discusses the aquatic environment at Lake Kizaki, central Japan, during the last ca. 60 years and describes the importance of laminated sediments in environmental analyses. The flux of total algal carbon increased between 1965 and 1996 while the BSi flux, which can be used in diatom production, showed a larger increase between 1960 and 1998 than typically occurs on average. The flux of dinosterol, an indicator of dinoflagellate production, also increased from 1966 to 1998, and the sedimentary dinoflagellate record correlated with observations of freshwater red tides caused by dinoflagellate blooms. Parallel laminated sediment was determined to have appeared between 1960 and 1995, corresponding to a period of high total algal carbon levels and BSi fluxes. For lamina formation and its preservation process, the thickness of the oxygen-poor layer depended on excessive total algal production during stagnant periods and appeared to be important because nutrients were diffused and accumulated in the oxygen-poor layer from bottom sediments. This could result in diatom blooms at the next overturn period. The development of the thick oxygen-poor layer appeared to be triggered primarily by the presence of excessive nutrients generated by human activities. In general, the occurrence of laminated sediments can provide a useful tool for understanding the eutrophic state in Lake Kizaki. 相似文献
69.
Hendrik Vogel Peter Rosén Bernd Wagner Martin Melles Per Persson 《Journal of Paleolimnology》2008,40(2):689-702
Measurements of Fourier transform infrared spectroscopy (FTIRS) in the mid-infrared (MIR) region were conducted on sedimentary
records from Lake El’gygytgyn, NE Siberia, and Lake Ohrid, Albania/Macedonia. Calibration models relating FTIR spectral information
to biogeochemical property concentrations were established using partial least squares regression (PLSR). They showed good
statistical performance for total organic carbon (TOC), total nitrogen (TN), and biogenic silica (opal) in the sediment record
from Lake El’gygytgyn, and for TOC, total inorganic carbon (TIC), TN, and opal in sediments from Lake Ohrid. In both cases,
the calibration models were successfully applied for down-core analysis. The results, in combination with the small amount
of sample material needed, negligible sample pre-treatments, and low costs of analysis, demonstrate that FTIRS is a promising,
cost-effective tool that allows high-resolution paleolimnological studies. 相似文献
70.
选取东海赤潮高发区常见的两种甲藻[东海原甲藻(Prorocentrum donghaiense)、塔玛亚历山大藻(Alexandrium tamarense)]和两种硅藻[中肋骨条藻(Skeletonema costatum)、海链藻(Thalassiosirasp.)],以2-苯基乙胺、腐胺、亚精胺、精胺四种赤潮水体中常见的生物胺为因素,设置0、5、25、100nmol/L四个浓度水平,进行L16(45)正交添加培养实验。根据Logistic生长模型进行曲线拟合,分析得到的生长参数。结果显示,不同的生物胺对各赤潮藻生长影响的大小、趋势均存在差异。其中,2-苯基乙胺对四种赤潮藻的生长影响最显著。高浓度的2-苯基乙胺对中肋骨条藻的生长具有明显的抑制作用,对塔玛亚历山大藻的生长具有明显的促进作用。多胺物质(腐胺、亚精胺和精胺)对甲藻(东海原甲藻和塔玛亚历山大藻)生长的促进作用大于硅藻(海链藻和中肋骨条藻)。多胺中的亚精胺对塔玛亚历山大藻和海链藻的生长影响最大,精胺对东海原甲藻和中肋骨条藻的生长影响最大。多胺可能是2010年东海赤潮由中肋骨条藻向东海原甲藻演替的一个诱导因素,其中精胺可能发挥的作用较大。 相似文献