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151.
Small granitic intrusions occur in the progressive metamorphic belts of the Chinese Ahai orogen. SHRIMP U-Pb analyses were performed on zircons separated from a tonalite intrusion and yielded a concordant age of 409.6±3.7 Ma ( MSWD = 0.93 ), restricting the emplacement and crystallization of the tonalite intru- sion to the Early Devonian. Combined with the existing geological data of the contemporary large granitic plutons in the Chinese Altai orogen, the tonalite is considered to be formed together with other granitic rocks in a continental arc setting. The tonalite intrusion has consistent foliation with its country rocks, indicating the strain resuiting in the regional deformation should be very strong during or after the early Devonian.  相似文献   
152.
井间干扰对煤层气渗流规律影响的数值模拟   总被引:1,自引:1,他引:0  
多井开采煤层气在我国尚处于起步阶段,该技术涉及的数学理论较为复杂,不易获得解析解,而数值模拟方法可以较好地获得数值解,从而为煤层气的开采提供理论指导。在基本假设条件下,建立了多井煤层气渗流数学模型;在一定的边界条件及初始条件下,利用数值模拟软件进行编程计算后,得到单井及多井开采100d后的压力场、压力漏斗降和速度场。数值模拟结果显示,在一定的生产区域和开采时间,随着井筒数目的增加,井间压力场和流速场干扰加强,压力漏斗降大面积扩展,煤层气供气区及解吸面积大幅增长,煤层气解吸能力及稳产能力加强。   相似文献   
153.
Palaeoflood hydrological study is a frontal subject of global change study. Using sedimentology, geomorphology and OSL dating methods, the typical palaeoflood slackwater deposits were studied in the Qishuihe River valley. The results showed that five flooding episodes with 21 palaeoflood events occurred during 4300–4250 a B.P., 4250–4190 a B.P., 4190–4100 a B.P., 4100–4000 a B.P. and 3100–3010 a B.P., respectively, during the Holocene period. The palaeoflood peak discharges were calculated with hydrological models. With a combination of the gauged flood, historical flood and palaeoflood hydrological data, the archives of flood events were extended to over 10,000 years in the Qishuihe River valley, and the flood frequency–peak discharge relationship curve was established accurately. These research results played important roles in mitigating flood hazard, hydraulic engineering and also the development of water resources in the semiarid Weihe River basin.  相似文献   
154.
泾河中游龙山文化晚期特大洪水水文学研究   总被引:21,自引:3,他引:18  
通过对泾河流域广泛深人的考察,在泾河中游彬县至永寿基岩峡谷河段发现典型的全新世古洪水平流沉积剖面,进行了古洪水沉积学和水文学研究.对于采集的全新世地层剖面序列样品,进行粒度成分、磁化率、烧失量、CaCO3,含量等分析,从沉积学角度证明了研究剖面所夹洪水沉积物具有平流沉积特征,为典型的洪水平流沉积物.根据地层学对比和剖面自身龙山文化晚期陶片、烧土等文化遗物分析,确定泾河在4200-4000 a BP发生了特大洪水事件,并利用沉积学和水文学原理恢复其水位,计算出古洪水洪峰流量为19490~22040 m3/s.同时,通过恢复现代大洪水、洪峰流量与流域面积关系对这种方法和古洪水洪峰流量计算结果进行了验证.不仅延长泾河洪水水文数据序列到万年尺度,而且为沿泾河的水利水电和交通工程建设及沿岸地区城镇的防洪减灾提供了重要的基础数据,具有重要的科学意义和应用价值.  相似文献   
155.
白穆  张勤  吴晓春 《测绘通报》2014,(12):82-85
从影像辐射质量和影像实际应用两个方面,对资源三号卫星影像数据的质量进行了评价与分析。影像辐射质量评价从辐射精度、信息度、清晰度、信噪比和纹理特征等方面进行,通过对比相近的ALOS卫星数据,结果显示资源三号卫星数据优于ALOS卫星数据;影像实际应用评价则通过秦岭地区1:25 000和1:50 000测图成果精度分析来进行,结果显示DEM高程精度、DEM平面精度和DLG采集精度均符合现行成果标准要求,可以满足国家基础比例尺测图要求。  相似文献   
156.
通过对汉江上游的野外考察,发现汉江上游郧西-郧县段第一级阶地前沿全新世土壤剖面中夹有多层古洪水滞流沉积物,选择该河段的归仙河口(GXH)剖面进行了详细野外观察,结合粒度成分和磁化率指标分析,证明它们是典型的古洪水滞流沉积物。采用石英的单片再生剂量法(SAR)获得了该剖面中9 个样品的光释光年龄值。基于测定的光释光年龄、考古断代和地层对比结果,确定这四期洪水事件分别发生在距今12500-12000 a、7500-7200 a、3100-2800 a,1000-900 a。通过与汉江上游地区、国内和世界各地的多种指标气候变化记录的对比分析,进一步探讨了汉江上游郧西郧县段全新世以来发生的多期古洪水事件发生的气候背景,这一认识有助于深入理解区域洪涝灾害对全球气候变化的响应规律。  相似文献   
157.
对汉江上游流域进行了深入的地层学及地貌学调查,在郧县河段河流一级阶地上覆黄土-古土壤沉积剖面中发现了典型的古洪水沉积层。对其进行了系统采样和粒度分析,结果表明,古洪水沉积层的粒度在空间上有明显的变化。水平方向上,相同层位的粒度自然分布曲线、概率累积曲线和平均粒径基本相同;垂直方向上,从上向下粒度自然分布曲线、概率累积曲线和平均粒径明显不同,粒径逐渐变细。水平方向上的粒度特征说明,古洪水同层位的样品可以相互替代;垂直方向上的变化与前人在泾河以及渭河流域等地研究发现的古洪水沉积层呈从下向上逐渐变细的沉积模式不同,说明古洪水沉积层的沉积模式并非只有一种,而是存在多种沉积模式,这种变化可能与洪水过程有关。  相似文献   
158.
以湖北庹家湾剖面为研究对象,对其宏观组构、沉积学及理化性质(磁化率、粒度、色度、元素组成等)进行了测试,用OSL方法进行了测年断代。根据野外和室内实验数据,建立了汉江Ⅰ级阶地上黄土-古土壤的地层序列,并以OSL测年数据为依据进行了地层年代学研究,利用气候替代指标重建了汉江上游55 ka BP以来气候变化的轨迹。认为:汉江Ⅰ级阶地在55 ka BP前后形成,阶地形成后即刻开始接受连续的风尘堆积;其地层从下向上依次分为L1-L3(55.0~28.5 ka BP)→L1-S2(28.5~24.5 ka BP)→L1-L2(24.5~23.0 ka BP)→L1-S1(23.0~21.0 ka BP)→L1-L1(21.0~11.5 ka BP)→Lt(11.5~8.5 ka BP)→S0(8.5~3.0 ka BP)→L0(3.0~0 ka BP);马兰黄土中记录了44.5~41.0 ka BP、37.5~34.0 ka BP、28.5~24.5 ka BP、23.0~21.0 ka BP四个暖湿气候阶段,其中28.5~24.5 ka BP和23.0~21.0 ka BP比较暖湿,形成了古土壤层L1-S2和L1-S1;庹家湾剖面记录的气候事件具有区域性特征,可与深海同位素曲线MIS-3进行良好比较,反映汉江地区MIS-3的后期暖湿程度较高;全新世大暖期(8.5~3.0 ka BP)在汉江上游地区并非一直表现为暖湿的特征,在5~6 ka BP出现短暂的相对凉湿的气候阶段。  相似文献   
159.
This paper presents the fiber-optic monitoring model and scheme for utilizing a fiber Bragg grating (FBG) sensor array to measure relative humidity. The effect of evaporation on reservoir rock involves various physical and chemical reactions under ambient laboratory conditions, which will result in a significant influence on the mechanical properties, especially for the surface of rock blocks in the fields. In this experiment, it was of great importance to better understand the effects induced by deionized water (DIW) evaporation occurring on the surface of a DIW-saturated sandstone core in terms of the induced small strains. The primary objective of this paper is to identify the applicability and feasibility of using the fiber Bragg grating sensors to monitor small strains induced by natural evaporation. This work also brings novel insights into the capability of high-precision measurements to predict the deformation mechanism of outcropped rocks, which often are subjected to natural evaporation. In this work, two arrays of fiber Bragg grating sensors were employed in the real-time monitoring of strain changes along the axial surface of a cylindrical sandstone core and to record the potential implications of the wavelength shifts induced by the evaporation factor. The experimental results could provide novel insights into the influences of natural evaporation on a rock monitored by FBG sensing technology under ambient laboratory conditions.  相似文献   
160.
A total of 118 of agricultural soil and 43 of vegetable samples were collected from Dongguan City, Guangdong, China. The spatial distribution, sources, accumulation characteristics and potential risk of heavy metals in the agricultural soils and vegetables were depicted in details by three different approaches, including total contents of eight metal elements in soils and vegetables, GIS maps and multivariate analysis of heavy metals in soils in the study. The results show that there are higher accumulation of heavy metals such as Cu, Zn, Ni, Pb, Cd and Hg in agricultural soils, and the contents of Pb (65.38 mg kg?1) and Hg (0.24 mg kg?1) are 1.82 and 2.82 times of the background contents of the corresponding heavy metals in soils of Guangdong Province, respectively. There are about 3.4% of Cu, 5.9% of Ni, 1.7% of Cd and 28% of Hg in all collected soil samples from all investigated sites which have overran the contents for heavy metals of the China Environmental Quality Standard for Soils (GB15618-1995, Grade Ⅱ). The pollution characteristics of multi-metals in soils are mainly reflected by Hg. There are different sources to eight metal elements in soils, Cu, Zn, Ni, Cr and As are predominantly derived from parent materials, and Pb, Hg and Cd are affected by anthropogenic activities. The spatial distribution shows that the Cu, Zn, Ni, Cr, Pb, As and Hg contents of agricultural soils are high in the west and low in the east, and Cd contents are high in the northwest, southeast and low in the southwest in Dongguan. The ratios of vegetable samples which Ni, Pb and As concentrations higher than the Maximum Levels of Contaminants in Foods (GB2762-2005) are 4.7%, 16.3% and 48.8%, respectively. The order of bio-concentration factors (BCF) of heavy metals in vegetables is Cd > Zn > Cu > As > Ni > Hg > Cr > Pb. It is necessary to focus on potential risk of heavy metals for food safety and human’s health from agricultural soils and vegetables in Dongguan City, Guangdong Province.  相似文献   
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