全文获取类型
收费全文 | 1496篇 |
免费 | 181篇 |
国内免费 | 300篇 |
专业分类
测绘学 | 25篇 |
大气科学 | 112篇 |
地球物理 | 393篇 |
地质学 | 495篇 |
海洋学 | 591篇 |
天文学 | 4篇 |
综合类 | 100篇 |
自然地理 | 257篇 |
出版年
2024年 | 7篇 |
2023年 | 31篇 |
2022年 | 62篇 |
2021年 | 63篇 |
2020年 | 67篇 |
2019年 | 87篇 |
2018年 | 54篇 |
2017年 | 57篇 |
2016年 | 53篇 |
2015年 | 74篇 |
2014年 | 97篇 |
2013年 | 114篇 |
2012年 | 83篇 |
2011年 | 92篇 |
2010年 | 92篇 |
2009年 | 93篇 |
2008年 | 93篇 |
2007年 | 75篇 |
2006年 | 98篇 |
2005年 | 76篇 |
2004年 | 78篇 |
2003年 | 50篇 |
2002年 | 69篇 |
2001年 | 44篇 |
2000年 | 28篇 |
1999年 | 43篇 |
1998年 | 25篇 |
1997年 | 22篇 |
1996年 | 27篇 |
1995年 | 12篇 |
1994年 | 9篇 |
1993年 | 18篇 |
1992年 | 8篇 |
1991年 | 6篇 |
1990年 | 7篇 |
1989年 | 3篇 |
1988年 | 5篇 |
1987年 | 4篇 |
1986年 | 6篇 |
1985年 | 15篇 |
1984年 | 9篇 |
1983年 | 9篇 |
1982年 | 6篇 |
1981年 | 5篇 |
1978年 | 1篇 |
排序方式: 共有1977条查询结果,搜索用时 31 毫秒
101.
Excessive terrestrial nutrient loadings adversely impact coral reefs by primarily enhancing growth of macroalgae, potentially leading to a phase‐shift phenomenon. Hydrological processes and other spatial and temporal factors affecting nutrient discharge must be examined to be able to formulate effective measures for reducing nutrient export to adjacent reefs. During storm events and baseflow periods, water samples were obtained from the tropical Todoroki River, which drains an intensively agricultural watershed into Shiraho coral reef. In situ nutrient analyzers were deployed for 6 months to hourly measure dissolved nutrient (NO3−‐N and PO43−‐P) concentrations. Total phosphorus (TP) and suspended solid concentration (TSS) were increased by higher rainfall intensity (r = 0·94, p < 0·01) and river discharge Q (r = 0·88, p < 0·01). In contrast, NO3−‐N concentration tends to decrease drastically (e.g. from 3 to 1 mg l−1) during flood events. When base flow starts to dominate afterwards, NO3−‐N manifested an increasing trend, but decreases when baseflow discharge becomes low. This counter‐clockwise hysteresis for NO3−‐N highlights the significant influence of groundwater discharge. N delivery can therefore be considered a persistent process compared to sediment and P discharge, which are highly episodic in nature. Based on GIS analysis, nutrient concentration along the Todoroki River was largely affected by the percentage of sugarcane/bare areas and bedrock type. The spatial distribution of N concentration in the river reflects the considerable influence of subsurface geology—higher N levels in limestone‐dominated areas. P concentrations were directly related to the total length of artificial drainage, which enhances sediment transport. The use of high‐resolution monitoring data coupled with GIS‐based spatial analysis therefore enabled the clarification of control factors and the difference in the spatio‐temporal discharge characteristics between N and P. Thus, although erosion‐reduction schemes would reduce P discharge, other approaches (e.g. minimize fertilizer) are needed to reduce N discharge. Copyright © 2010 John Wiley & Sons, Ltd. 相似文献
102.
A. V. Pavlov 《Pure and Applied Geophysics》1988,127(2-3):529-544
Theoretical and experimental aspects of the production, transformation, diffusion and loss of N2 in the upper atmosphere are considered. The N2-CO2 near-resonant system in theD andE regions is taken into account. We describe our understanding of the methods necessary to find the vibrational populations of N2 and CO2 (asymmetric mode of CO2). The calculations of the vibrational temperatures in theD, E, andF regions for the mid-latitude ionosphere and an aurora are presented. The connection between the excited species and the 4.26-m radiation intensities is considered. The models for the rate coefficient of the reaction of O+ with N2 and the electron density decrease resulting from N2 in the F region are discussed. 相似文献
103.
Knut L. Seip 《Aquatic Sciences - Research Across Boundaries》1994,56(1):16-28
Regression results based on data from 46 northern temperate lakes show that total phosphorus (TP) is the best predictor for phytoplankton (as chl-a) at lower trophic levels, TP < 200 mg · m–3. A regression including both TP and TN as regressors is the best predictor for lakes with TP > 200 mg · m–3. However, the good correlation is probably due to a high correlation between lake average chl-a (all years observed) and lake average TP and TN. Within single hypereutrophic lakes, TN alone is the best predictor. It was not possible to identify a medium trophic domain where TN and TP in combination was the best predictor for chl-a. The ratio TN:TP in the water decreases from about 40 to about 5 with increasing trophic level. Optimum TN:TP ratio for algal species with high abundance during late summer and autumn reflects this decreasing ratio, but within a lesser range, i.e., 20 to 5. In contrast, TN:TP ratios for species abundant during the early vernal period showed no, or an inverse, relation to the TN:TP ratio of the water. 相似文献
104.
Historical changes in sediments of Pyramid Lake,Nevada, USA: consequences of changes in the water balance of a terminal desert lake 总被引:1,自引:0,他引:1
Sediment cores from the shallow and deep basins of Pyramid Lake, Nevada, revealed variations in composition with depth reflecting changes in lake level, river inflow, and lake productivity. Recent sediments from the period of historical record indicate: (1) CaCO3 and organic content of sediment in the shallow basin decrease at lower lake level, (2) CaCO3 content of deep basin sediments increases when lake level decreases rapidly, and (3) the inorganic P content of sediments increases with decreasing lake volume. Variations in sediment composition also indicate several periods for which productivity in Pyramid Lake may have been elevated over the past 1000 years. Our data provide strong evidence for increased productivity during the first half of the 20th Century, although the typical pattern for cultural eutrophication was not observed. The organic content of sediments also suggests periods of increased productivity in the lake prior to the discovery and development of the region by white settlers. Indeed, a broad peak in organic fractions during the 1800's originates as an increase starting around 1600. However, periods of changing organic content of sediments also correspond to periods when inflow to the lake was probably at extremes (e.g. drought or flood) indicating that fluctuations in river inflow may be an important factor affecting sediment composition in Pyramid Lake. 相似文献
105.
采用了单柱离子色谱法测MnO2产品中无机离子杂质;提出了消除干扰的可行途径,将La(OH)3加入后能同时消除进样峰的干扰和溶剂峰的出现。选用1.75mmol/L邻苯二甲酸1.75mmol/L三羟甲基氨基甲烷为混合淋洗剂测定F^-,Cl^-,NO3^和SO^2-4,其标准加入回收率为95%-105%;RSD(n=7)为2.47%-8.08%。 相似文献
106.
Amino acid nitrogen in atmospheric aerosols: Occurrence,sources and photochemical modification 总被引:2,自引:0,他引:2
The presence of amino acids in atmospheric precipitation and aerosols has been noted for many years, yet relatively little is known about these or other nitrogen containing organic compounds in the atmosphere. Marine and continental rainwater analyses indicate that atmospheric aerosols, and subsequently atmospheric precipitation, may contain substantial levels of free and combined amino acids. The most likely source of amino N in the remote marine atmosphere appears to be the injection of proteinaceous material through the action of bursting bubbles at the sea-air interface or the long range transport from terrestrial sources. The capacity of these substrates to undergo photooxidation and photodegradation in the atmosphere to simpler species, such as ammonium ions, carboxylic acids, and for the S containing amino acids, oxidized forms of sulfur, has received little attention from atmospheric chemists. The photochemistry of covalently bound amino groups, particularly as found in peptides and amino acids, is discussed here with the purpose of summarizing what is known of their occurrence and their possible importance to atmospheric chemistry. 相似文献
107.
108.
无机增强纤维Ⅰ.钛酸钾纤维 总被引:9,自引:0,他引:9
结晶质的钛酸钾纤维因其性质特殊而备受青睐,本文介绍了二钛酸钾、四钛酸钾、六钛酸钾和八钛酸钾纤维的结构、性质、用途,及国内外的研究现状. 相似文献
109.
Wolfgang Junkermann Ulrich Platt Andreas Volz-Thomas 《Journal of Atmospheric Chemistry》1989,8(3):203-227
Photoelectric detectors for the measurement of photolysis frequencies of different trace gases in the atmosphere are described. They exhibit uniform response characteristics over one hemisphere (2 sr) and wavelength characteristics closely matched to those of the photolysis frequencies J
O1D, J
NO2, and J
NO3, respectively. Absolute calibration of the J
O1D detector was performed by chemical actinometry with an accuracy of ±16 percent. Simultaneous measurements of J
NO2 and J
O1D are presented. 相似文献
110.
S. Madronich D. R. Hastie B. A. Ridley H. I. Schiff 《Journal of Atmospheric Chemistry》1984,1(2):151-157
The photodissociation coefficient, J
NO2 of NO2 in the atmosphere was calculated at 235 and 298 K using the measured temperature dependences of the absorption cross-sections and quantum yields. These calculations gave a ratio J
NO2(298 K)/J
NO2(235 K)=1.155±0.010 which is only weakly dependent on altitude, surface albedo and solar zenith angle. 相似文献