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981.
982.
983.
Trophic Assessment in Chinese coastal systems-review of methods and application to the Changjiang (Yangtze) Estuary and Jiaozhou Bay 总被引:3,自引:0,他引:3
Yongjin Xiao João G. Ferreira Suzanne B. Bricker João P. Nunes Mingyuan Zhu Xuelei Zhang 《Estuaries and Coasts》2007,30(6):901-918
Coastal eutrophication has become one of the main threats to Chinese coastal areas during the last two decades. High nutrient
loads from human activities have modified the natural background water quality in coastal water bodies, resulting in a range
of undesirable effects. There is a need to assess the eutrophic level in coastal systems and to identify the extent of this
impact to guide development of appropriate management efforts. Traditional Chinese assessment methods are discussed and compared
with other currently-used methods, such as the Oslo-Paris Convention for the Protection of the North Sea (OSPAR) Comprehensive
Procedure and Assessment of Estuarine Trophic Status (ASSETS). The ASSETS method and two Chinese methods were tested on two
Chinese systems: the Changjiang (Yangtze) Estuary and Jiaozhou Bay. ASSETS is process based, and uses a pressure-state-response
model based on three main indices: Influencing Factors, Overall Eutrophic Condition, and Future Outlook. The traditional methods
are based on a nutrient index. ASSETS was successfully applied to both systems, classifying the Changjiang Estuary as Bad
(high eutrophication) and Jiaozhou Bay as High (low eutrophication). The traditional methods led to ambiguous results, particularly
for Jiaozhou Bay, due to the high spatial variability of data and a failure to assess the role of shellfish aquaculture in
nutrient control. An overview of the Chinese coastal zone identifies 50 estuaries and bays that should form part of a national
assessment. A comparison of methods and results suggests that ASSETS is a promising tool for evaluating the eutrophication
status of these systems. 相似文献
984.
Tao Li Zhe Zhu Dongsheng Wang Chonghua Yao Hongxiao Tang 《International Journal of Mineral Processing》2007
Flocs generated by various shear forces exhibit different characteristics of size, strength and structure. These properties were investigated by employing a continuous optical monitoring and a microscope with CCD camera to directly monitor aggregation under six different shear intensities. The floc structure was characterized by the fractal dimension. The results showed that the flocculation index (FI) decreased from 1.16 at 20 rpm to 0.25 at 250 rpm and the floc size decreased from 550 μm to 150 μm, meantime, the FI value showed a good correlation with floc size. In order to determine the floc strength, two methods were used. One was the strength factor, ranging from 18.3% to 62.5%, calculated from FI curve, and the other was a theoretical value between 0.005 N/m2 and 0.240 N/m2, estimated by calculation. The floc strength increased with the G value in both cases. Furthermore, the fractal dimension increased with G and its value was between 1.30 and 1.63. The relation between fractal dimension and strength was also obtained. 相似文献
985.
986.
987.
湖南洞庭湖地区土壤中Hg的来源 总被引:1,自引:0,他引:1
Hg污染已成为全球性的环境问题,尤其是Hg对土壤的污染,因其具有隐蔽性、不可逆性和长期性的特点,对陆生生态系统构成潜在的巨大威胁,因此查明土壤中Hg的来源非常重要。运用生态地球化学填图的指导思想,对湖南洞庭湖地区土壤剖面分析和成土过程研究后发现,表层土壤中Hg含量的高低与成土母质中Hg的含量有很好的对应性,成土过程对土壤中Hg的含量也有显著的影响。 相似文献
988.
989.
根据显微镜观察,塔里木盆地砂岩储层中SiO2溶蚀分为石英颗粒边缘溶蚀、次生加大边溶蚀和交代溶蚀。通过对石英颗粒和加大边溶蚀特征及其与粘土矿物组合、与碳酸盐胶结、与古油藏破坏以及现今油田水中Si离子含量等关系的综合研究,这些SiO2溶蚀可能存在两种机理:碱性环境下的SiO2溶蚀和有机酸(烃类微生物降解产生的有机酸以及有机质成熟产生的有机酸)引起的SiO2溶蚀。第一种溶蚀类型较普遍,但程度微弱;第二种溶蚀类型主要发生在古油藏破坏和有机质成熟过程中,这种溶蚀较强烈但很局限。SiO2的溶蚀作用可以为油气提供一定量的储集空间,这对于深埋的时代较老的志留-泥盆系储层具有重要意义。在古油藏中尽管烃类已经充注储层孔隙,但只要孔隙中存在有机酸或碱性孔隙水,SiO2的溶蚀和石英次生加大的胶结等作用仍可进行。 相似文献
990.
Simulation experiments on the primary migration of oil were carried out on massive samples. The results proved that oil generated from source rocks was expelled in the form of an independent oil phase. High oil-expulsion efficiency was observed. It follows that the primary migration of oil is not directly dependent on the quantity of oil generated from the source rocks. Therefore, the oil-expulsion proportion was high though some source rocks yielded only a limited amount of oil. A great deal of gas was produced at the same time of oil-generation. Thus, it can be concluded that the main expulsion energy for oil primary migration came from these gases. 相似文献