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92.
A study of interaction between surface water and groundwater using environmental isotope in Huaisha River basin 总被引:20,自引:0,他引:20
The surface water and groundwater are important components of water cycle, and the interaction between surface water and groundwater is the important part in water cycle research. As the effective tracers in water cycle research, environmental isotope and hydrochemistry can reveal the interrelationships between surface water and groundwater effectively. The study area is the Huaisha River basin, which is located in Huairou district, Beijing. The field surveying and sampling for spring, river and well water were finished in 2002 and 2003. The hydrogen and oxygen isotopes and water quality were measured at the laboratory. The spatial characteristics in isotope and evolution of water quality along river lines at the different area were analyzed. The altitude effect of oxygen isotope in springs was revealed, and then using this equation, theory foundation for deducing recharge source of spring was estimated. By applying the mass balance method, the annual mean groundwater recharge rate at the catchment was estimated. Based on the groundwater recharge analysis, combining the hydrogeological condition analysis, and comparing the rainfall-runoff coefficients from the 1960s to 1990s in the Huaisha River basin and those in the Chaobai River basin, part of the runoff in the Huaisha River basin is recharged outside of this basin, in other words, this basin is an un-enclosed basin. On the basis of synthetically analyses, combining the compositions of hydrogen and oxygen isotopes and hydrochemistry, geomorphology, geology, and watershed systems characteristics, the relative contributions between surface water and groundwater flow at the different areas at the catchments were evaluated, and the interaction between surface water and groundwater was re- vealed lastly. 相似文献
93.
采用水化学仪器自动记录、现场滴定和样品碳氧稳定同位素测试相结合等方法,对云南中甸白水台钙华景区的水化学和碳氧稳定同位素特征进行了综合分析。主要结论是:形成白水台钙华的泉水具有很高的钙和重碳酸根离子浓度,相应地,泉水的CO2分压显著高于土壤生物成因所能产生的CO2分压。结合泉水出露的地质条件及其碳稳定同位素特征(δ13C=-1.23‰)的分析,进一步发现,高CO2分压主要与深部地热成因的CO2有关,而非原来普遍认为的“是温暖湿润气候的产物”。可见,白水台钙华属于热成因类钙华。由此,根据白水台不同时代钙华氧稳定同位素组成的差异,对钙华形成时的水温进行了计算。结果发现自白水台钙华形成以来,水温变化高达11℃,即从最老(<35万年)钙华形成时的21℃降至现在的10℃。这可能与本地区强烈抬升导致的气温降低有关,也可能反映出地热对水温的影响在降低。此外,本文对用热成因类钙华进行古环境重建研究中值得注意的问题也做了讨论。这些问题包括放射性碳测年中“死碳”(来自深部碳酸盐碳和深部CO2)的干扰及由深源CO2和CO2自水中逸出导致的钙华13C富集,后者在利用类似热成因碳酸盐沉积的δ13C进行古植被重建时也是必须考虑的问题 相似文献
94.
Salt-water intrusion and nitrate contamination in the Valley of Hermosillo and El Sahuaral coastal aquifers, Sonora, Mexico 总被引:1,自引:0,他引:1
The Valley of Hermosillo coastal aquifer, state of Sonora, northwestern Mexico, has been over-exploited for the last four
decades, in order to maintain agricultural activity in one of the most important irrigation districts of the Mexican Republic.
The over-exploitation has resulted in the development of several drawdown cones and in the lowering of the water table to
as much as 50 m below mean sea level. Contamination of the aquifer in the form of salt-water intrusion from the Gulf of California
and high nitrate concentrations is the consequence of human activities. A hydrogeochemical zonation of the aquifer, based
on the presence of different water families, led to the identification of a coastal band approximately 30 km wide that is
affected by salt-water intrusion. Conductivity of the sampled water and the interpretation of the ratio Na/Cl×1000 was used
to identify the location of three major intrusion plumes in this coastal band. The background nitrate contamination of the
aquifer is about 4 ppm, but contents as great as about 17 ppm occur in some wells. Irrigation with raw sewage and movement
of contaminants in areas of high hydraulic gradients within the drawdown cones probably are responsible for localized peaks
of the nitrate concentration.
Received, October 1996 Revised, September 1997, May 1998 Accepted, July 1998 相似文献
95.
唐古拉山冬克玛底冰川作用区的水化学特征 总被引:8,自引:6,他引:8
冬克玛底冰川附近地区是该冰川化学成分的主要来源区。冬克玛底河水及冰川上的新,老雪的矿化度,总碱度,硬度的大小顺序是:河水-老雪--新雪。虽然它们都属淡水范畴,但新雪是性偏酸的极软水,老雪是偏碱的极软水,河水则属碱性软水。 相似文献
96.
97.
98.
99.
以京西杨坨煤矿的试验为例,概述了应用环境同位素和其它水化学成分研究矿井突水来源的成果。为矿井防治水提供了可靠依据。 相似文献
100.
淮北临涣矿采煤沉陷区不同水体水化学特征及其影响因素 总被引:3,自引:0,他引:3
为研究淮北临涣矿采煤沉陷区不同水体的补给水源及溶质来源,在现场调查的基础上,系统采集丰水期、平水期、枯水期沉陷区积水、地表河水和浅层地下水样进行测试分析,采用Piper三线图、Gibbs图和因子分析方法,对不同水体水化学特征及其影响因素进行讨论.结果表明:地表水水体总溶解性固体(TDS)质量浓度表现为枯水期丰水期平水期,浅层地下水表现为枯水期平水期丰水期,地表水TDS质量浓度明显高于浅层地下水.地表水中主要阴阳离子为Na~+、Cl~-和SO_4~(2-),水化学类型主要为SO_4~(2-)-Cl~--Na~+型;浅层地下水离子以HCO_3~-、Ca~(2+)和Mg~(2+)为主,表现为HCO_3~--Ca~(2+)-Mg~(2+)型.结合Gibbs图和因子分析可知,地表水受蒸发作用、地表径流以及采煤活动等因素影响,浅层地下水在一定程度上体现出大气降水和地表水补给的特点,受岩石风化作用影响较为明显. 相似文献