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51.
针对吉林市铁合金厂排污口下游江水的污染情况,设计研究江段,分段、分层取样。通过野外与室内实验,分析研宄了江水污染物的主要成分,并对NH4^ 的纵向、横向、垂向上的分布特征及其影响因素进行了详细研究。结果表明,垂直方向污染物扩散可以瞬时完成,在极短的时间内基本能达到完全混合;在横向和纵向上,岸边排放污染物一般只在近岸扩散,污染范围一般也只在靠近排污口一带;随着离排污口距离增大,污染物浓度降低,横向变化率较纵向大。本研究为排污口的污染物控制与治理、水资源保护提供了科学依据。 相似文献
52.
The paper summarises the history of human settlement in the Sudetes from the Bronze Age. A more intensive stage was reached
in the Middle Ages when settlers from the west established new villages deep in the mountain valleys. By the beginning of
the 20th century the Sudetes were already overpopulated but after a near-complete ethnic replacement from a German to a Polish
population in 1945–8, population continued to grow until the 1980s. However, the economic system was hardly sustainable by
this time. There were many polluting industries in the region and massive transboundary pollution from adjacent areas of Czechoslovakia
and Germany had a devastating effect on the forests. Moreover, subsidised state agriculture placed heavy pressure on vulnerable
mountain grazings. Since 1989 there has been a process of deindustrialisation in the Sudetes and surrounding areas and, with
the disappearance of the state farms and the reduction in subsidies, agriculture is now better adjusted to the natural potential
and is complemented by a promising start with agrotourism. The population of the region is growing relatively slowly (0.8%
per annum 1956–1999), with the rural areas now in decline. A sustainable future for the region is now a possibility, but while
there is a consensus for continued environmental reconstruction, supported by alternative economies, this will have to be
carefully managed in the years ahead when EU accession may bring heavier development pressures than those evident at the moment.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
53.
锑矿区水体水环境锑污染及硫同位素示踪研究 总被引:4,自引:0,他引:4
本文系统研究了贵州省半坡锑矿区水环境锑污染现状,用硫同位素指示采矿活动对矿区水体的影响,以查明锑矿区水环境中Sb的释放迁移过程和水污染程度。研究发现,矿区水体中Sb和SO42-含量分别高达1377μg/L和1926 mg/L;岔河下游近10 km处仍保持较高水平(182.5μg/L Sb和59.8 mg/L SO42-)。岔河水体中,δ34S-Sb、δ34S-SO42-和Sb-SO42-间均具显著正相关,相关系数分别为r=0.68(p<0.05)、r=0.89(p<0.01)、r=0.72(p<0.05)。表明岔河水体中,δ34S和SO42-能很好地指示矿业活动引起的Sb污染程度和扩散范围。根据同位素质量平衡原理估算,发现矿区下游水体中的硫主要来自矿山,表明矿区下游水体污染受采矿活动影响显著。 相似文献
54.
Claude Boutron Kevin Rosman Carlo Barbante Michael Bolshov Freddy Adams Sungmin Hong Christophe Ferrari 《Comptes Rendus Geoscience》2004,336(10):847-867
The investigation of the occurrence of lead in dated snow and ice from Greenland and Antarctica has played a major role in our understanding of the history of the pollution of the atmosphere of our planet by this metal. Such studies have however proved to be very demanding, mainly because of the extreme purity of polar snow and ice. Reliable measurements can be obtained only if ultra-clean and highly sensitive procedures are used, as pioneered by Clair Patterson. The Greenland data show evidence of large-scale pollution of the atmosphere of the Northern Hemisphere for lead as early as two millennia ago during Greco–Roman times, especially because of mining and smelting activities in southern Spain. It peaked at the end of the 1960s, with lead concentrations in snow about 200 times higher than natural values, before declining during recent times because of the fall in the use of leaded gasoline. Lead pollution in Antarctica was already significant at the end of the 19th century as a consequence of whaling activities, the traffic of coal-powered ships crossing the Cape Horn, and mining activities in South America, South Africa and Australia. After declining because of the opening of the Panama Canal, the great economic depression and World War II, it reached a maximum during the 1980s, with lead concentrations 20 times higher than natural values. Other studies focus on past natural variations of lead in ancient ice dated from the last climatic cycles. To cite this article: C. Boutron et al., C. R. Geoscience 336 (2004). 相似文献
55.
In the present investigation, an effort has been made to identify the critical sub-watersheds for the development of best
management plan for a small watershed of Eastern India using a hydrological model, namely, AVSWAT2000. A total of 180 combinations
of various management treatments including crops (rice, maize ground nut and soybean), tillage (zero, conservation, field
cultivator, mould board plough and conventional practices) and fertilizer levels (existing half of recommended and recommended)
have been evaluated. The investigation reveled that rice cannot be replaced by other crops such as groundnut, maize, mungbean,
sorghum and soybean since comparatively these crops resulted in higher sediment yield. The tillage practices with disk plough
have been found to have more impact on sediment yield and nutrient losses than conventional tillage practices for the existing
level of fertilizer. Sediment yield decreased in the case of zero tillage, conservation tillage, field cultivator, moldboard
plough, and conservation tillage as compare to conventional tillage. Lowest NO3–N loss was observed in zero tillage in all the fertilizer treatments, whereas field cultivator, moldboard plough and disk
plough resulted in increase of NO3–N loss. As compared to conventional tillage, the losses of soluble phosphorus were increased in moldboard plough. The losses
of organic nitrogen were also increased as fertilizer dose increased. After zero tillage the conservation tillage preformed
better in all the fertilizer treatments as per loss of organic nitrogen and organic phosphorus is concerned. It can be concluded
that the sediment yield was found to be the highest in the case of disk plough followed by moldboard plough, field cultivator,
conventional tillage, field cultivator and least in zero tillage practices. The nutrient losses were found to be in different
order with tillage practices, resulted highest in disk plough tillage practices. In view of sediment yield and nutrient losses,
the conservation tillage practice was found to be the best as the sediment yield is less than the average soil loss whereas
nutrient loss is within the permissible limit. 相似文献
56.
利用元素总量和Pb同位素示踪技术对广东云浮硫酸厂含Tl黄铁矿冶炼堆渣场周围土壤中Tl的污染程度和迁移行为进行了研究。研究发现堆渣场周围土壤中Tl污染物主要集中于表层土壤约16.5cm深度内,并且表现出沿垂直方向向下迅速下降的特点。堆渣场周围土壤中Tl与Pb呈显著线性相关,表明自然条件下田与Pb在土壤中的迁移相似性,并且都以横向迁移为主。堆渣场固结层周围土壤至少44cm范围已经受到废渣中Tl释放的影响,Tl污染物平均下渗速率达到2.75cm/a。酸性雨水的淋滤作用及废渣自身不断酸化的特性是废渣中.Tl迁移释放入土壤的主要因素,土壤铁氧化物胶体及有机质是土壤对Tl产生吸附的主要载体。 相似文献
57.
58.
柱撑蛭石吸附去除废水中重金属离子的实验研究 总被引:2,自引:0,他引:2
分别利用有机柱化剂十二烷基磺酸钠(SDS)和无机柱化剂聚羟基铝(HA)对蛭石进行柱撑制得十二烷基磺酸钠柱撑蛭石(SDS-V erm icu lite)和聚羟基铝柱撑蛭石(HA-V erm icu lite),并通过XRD、红外光谱、ZETA电位等表征手段对柱撑蛭石进行表征,同时针对柱撑蛭石对Cu2 ,Cd2 ,C r3 3种重金属离子的吸附进行研究,结果表明:吸附去除率受反应时间、重金属离子的初始浓度、pH值等因素的影响,经柱撑后的蛭石对重金属离子吸附的吸附性能比蛭石原矿要强。柱撑蛭石吸附3种重金属离子的动力学吸附过程可用E lov icb方程和双常数方程进行较好的拟合。 相似文献
59.
为了弄清楚煤矸石回填地基对复垦区的环境效应,以开滦矿区吕家坨复垦新村为例,介绍了地基回填煤矸石工艺,分析了煤矸石化学成分及其含量;采用室内淋溶实验,对pH、总硬度(CaCO3)、F^-、SO4^2-、Pb、Cd和Cr^6+浓度等地下水环境质量指标进行分析,探讨了煤矸石回填地基对水环境的影响;讨论了煤矸石回填地基对大气质量的影响;参照《城市放射性废物管理办法》规定,评价了回填地基煤矸石的放射性对人体健康的危害。结果表明:通过现场振动压实试验确定了回填地基分层充填、分层振动压实参数及碾压趟数,确定按照煤矸石与土体积之比5:2进行回填,若回填一层厚500mm煤矸石,则要回填一层厚200mm粉煤灰或土,地表覆土厚度确定为0.5m;煤矸石中SiO2和Al2O3含量较高,属基性岩类,同时煤矸石含有炭、铝和CaO等物质,易发生水解和风化等现象;地基分层回填压实的复垦工艺减少了煤矸石中有害物质的释放量,降低了污染物的迁移速度,不会对水环境造成污染;地基回填煤矸石也显著减少粉尘和有害气体的排放量,降低对大气的污染;研究区煤矸石不属于放射性废物,不会影响人体健康,可作为建筑材料使用。 相似文献
60.
乌鲁木齐河源1号冰川表层雪的化学特征——以低分子有机酸和无机阴离子为例 总被引:3,自引:0,他引:3
表层雪是联系大气成分与冰芯记录的重要纽带,是研究成冰作用过程中化学组成变化的起点.为配合天山乌鲁木齐河源1号冰川成冰作用过程中化学组成变化的研究,对1号冰川积累区(海拔4130 m)一个完整年度的表层雪样品进行了低分子有机酸和无机阴离子含量的分析.结果显示:表层雪中低分子有机酸主要有HCOO-、CH3COO-、C2H5COO-和(COO)22-,无机阴离子主要有F-、Cl-、NO2-、NO3-、SO42-和PO43-.除(COO)22-外,大部分高浓度的有机酸和无机阴离子因受到周围环境和盛行风的影响呈现出明显的季节变化特征,即夏半年离子浓度变化剧烈,最大值和最小值同时出现在夏半年,冬半年的浓度则相对小而稳定;而(COO)22-和低浓度的无机阴离子随季节变化的特征不明显,在全年均显示出波动性.在外界条件不变的情况下,表层雪可以长时间(至少半年时间)保存其中高含量的化学组成不被改变. 相似文献