全文获取类型
收费全文 | 254篇 |
免费 | 73篇 |
国内免费 | 97篇 |
专业分类
测绘学 | 38篇 |
大气科学 | 46篇 |
地球物理 | 61篇 |
地质学 | 165篇 |
海洋学 | 42篇 |
综合类 | 29篇 |
自然地理 | 43篇 |
出版年
2024年 | 2篇 |
2023年 | 15篇 |
2022年 | 29篇 |
2021年 | 39篇 |
2020年 | 31篇 |
2019年 | 35篇 |
2018年 | 18篇 |
2017年 | 20篇 |
2016年 | 12篇 |
2015年 | 16篇 |
2014年 | 21篇 |
2013年 | 25篇 |
2012年 | 16篇 |
2011年 | 16篇 |
2010年 | 21篇 |
2009年 | 11篇 |
2008年 | 18篇 |
2007年 | 12篇 |
2006年 | 9篇 |
2005年 | 3篇 |
2004年 | 5篇 |
2003年 | 6篇 |
2002年 | 8篇 |
2001年 | 6篇 |
2000年 | 5篇 |
1999年 | 6篇 |
1998年 | 5篇 |
1997年 | 2篇 |
1996年 | 2篇 |
1995年 | 3篇 |
1994年 | 1篇 |
1993年 | 1篇 |
1992年 | 1篇 |
1991年 | 1篇 |
1988年 | 3篇 |
排序方式: 共有424条查询结果,搜索用时 31 毫秒
151.
152.
为了深入探究不同煤岩类型储渗空间的特征及其差异性,选取了韩城矿区4种不同煤岩类型的中煤阶样品,采用低
场核磁共振技术,实现了对韩城矿区不同煤岩类型孔裂隙的识别和有效孔隙度差异性的精细描述和定量表征,并在此基础
上基于离心前后累计振幅曲线求取了孔裂隙系统划分的阀值T2C1和T2C2,实现了对不同煤岩类型孔径结构分布的重构。实验
结果表明:不同煤岩类型煤样的T2谱形态差异较大,从光亮煤到暗淡煤,T 2谱由双峰大孔隙型逐渐过渡到双峰小孔隙型,
且T2C截止值和有效孔隙度均呈现出逐渐降低的趋势;并由求取的阀值T2C1和T2C2计算得到的三大孔裂隙系统孔径分布可知,
从光亮煤到暗淡煤,储层的孔裂隙结构由渗流孔型逐渐向综合型和扩散孔型过渡。 相似文献
153.
154.
155.
Dissolved organic matter (DOM) from riverine and lacustrine water was isolated using a reverse osmosis (RO) system. Solid-state 13C nuclear magnetic resonance (13C NMR) was used to quantitatively evaluate the compositions and constituents of DOM, which are compared with previous investigations on marine DOM. Results indicated that concentration factor (CF) was a key metric controlling yield and sorption of DOM on the RO system. The sorption was likely non-selective, based on the 13C NMR and δ13C analyses. Carbohydrates and lipids accounted for 25.0–41.5% and 30.2–46.3% of the identifiable DOM, followed by proteins (18.2–19.8%) and lignin (7.17–12.8%). The freshwater DOM contained much higher alkyl and aromatic C but lower alkoxyl and carboxyl C than marine DOM. The structural difference was not completely accounted for by using structure of high molecular weight (HMW) DOM, suggesting a size change involved in transformations of DOM during the transport from rivers to oceans. 相似文献
156.
A pioneering investigation of semi‐volatile organic compounds (SVOCs) in shallow groundwater in China was hereby reported. Representative groundwater samples were collected from three selected regions: Eastern Hai River Plain, Yangtze River Delta, and Yunnan‐Guizhou Plateau, and analyzed for 103 SVOCs linked to agricultural and industrial practices. Analytical results showed that 70 of the 103 SVOCs were present in the groundwater samples, a detection frequency of approximately 86%. Compounds detected most frequently included P,P′‐DDT (53.49%, MDL 0.0007 µg/L), 2,4‐dinitrotoluene (51.16%, MDL 0.02 µg/L), and phenol (51.16%, MDL 0.02 µg/L). Fifteen SVOCs, such as P,P′‐DDT, 2,4‐dinitrotoluene, heptachlor, and aldrin, were detected at concentrations exceeding the USA National Recommended Water Quality Criteria‐2009 (USNRWQC‐2009). Most of these 15 SVOCs belong to polycyclic aromatic hydrocarbons and organochlorine pesticides. The detection of SVOCs in the Yunnan‐Guizhou Plateau warrants special concern, since this region has limited human activities and been assumed as an environmentally pristine area. The data from this work are expected to contribute to the database of contemporary groundwater quality in China. 相似文献
157.
158.
"伊布都"台风影响云南的暴雨过程分析 总被引:24,自引:13,他引:11
利用Micaps常规资料,采用FY-2卫星红外增强云图及昆明CINRAD-CC雷达资料,分析了2003年7月25日20:00~26日20:00由于“伊布都”台风低压西行引发的云南暴雨过程。结果表明,由于副热带高压的西伸加强,其西侧持续强盛的低空偏南急流使西移到云南的热带低压维持并加强,在此有利的大尺度背景下,使云南境内的台风低压云系由MβCS发展为MαCS-MCC;通过K指数、θse特征、非地转湿Q矢量及非地转湿Q矢量散度等的分析,发现高能、高湿不稳定能量的积聚、低层的水汽辐合是此次暴雨过程的触发机制;地形的抬升导致低压发展,是暴雨产生的重要原因之一;多普勒雷达回波显示,台风低压有明显较大尺度的气旋式螺旋带状回波结构,并伴有多条强回波短带的出现及合并;在多普勒雷达速度图上,逆风区、气旋式辐合、大风区、持续的暖平流是造成本次暴雨过程直接的中小尺度天气系统。 相似文献
159.
Chemical weathering in Luzon, Philippines from clay mineralogy and major-element geochemistry of river sediments 总被引:3,自引:0,他引:3
Zhifei Liu Yulong Zhao Christophe Colin Fernando P. Siringan Qiong Wu 《Applied Geochemistry》2009,24(11):2195-2205
Clay mineralogy and major-element geochemistry of 35 surface sediment samples collected in 21 major to moderate rivers of Luzon, Philippines are used to evaluate the present chemical weathering process. The clay mineral assemblage consists mainly of smectite (average 86%) with minor kaolinite (9%) and chlorite (5%) and very scarce illite (1%), and does not show strong island-wide differences. The major element results of both bulk and clay-fraction sediments indicate that the formation of clay minerals is accompanied by leaching of Ca and Na first and of Fe and Mn thereafter during the chemical weathering process. A low-moderate chemical weathering degree of bulk sediments and a moderate-intensive degree of clay-fraction sediments are obtained in Luzon rivers based on proxies of chemical index of alteration (CIA) and smectite crystallinity. It is suggested that the majority of andesitic–basaltic volcanic and sedimentary rocks along with the tectonically active geological setting and sub-tropical East Asian monsoon climate are responsible for the predominance of smectite in the clay mineral assemblage. 相似文献
160.
为了探究水文地质结构对地下水流数值模拟的不确定性,可以运用随机模拟建立地下水位的预测模型。根据转移概率地质统计方法模拟多孔介质岩性分布,利用非线性规划的思路计算岩性与水文地质参数之间的关系,从而建立相对精确的随机水文地质参数场。将不同的水文地质参数场运用到MODFLOW中,得到不同的随机模拟结果。通过比较随机模型和确定模型的末流场拟合情况以及水位动态拟合图,发现确定模型和随机模型具有相似趋势,都能与实测流场拟合较好,但是随机模型更能体现真实的水文地质特征。对随机模型预测10年后的地下水水位做不确定性分析,得到水位平均变幅介于-5~5 m之间,且95%置信度水位变幅的平均上限线约为0.146 m。研究结果为决策者提供科学依据。 相似文献