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921.
土壤水全时空调控的初步探讨 总被引:3,自引:1,他引:2
农业是第一用水大户,有利利用土壤是实现黑龙港地区农业可持续发展的关键,本文分析了黑龙港地区主要作物需水与降水的关系,建立了作物生长条件包气带流动系统的概念,并以此为基础提出了土壤水全时空调控的概念,探讨了土壤水全时空调控的涵义与措施,指出土壤水调控是一系统工程,必须多种措施有机结合,简单介绍了王瞳试验场开展的田间土壤水调控试验成果。 相似文献
922.
活动断裂带的壤中气汞量测量研究 总被引:2,自引:0,他引:2
在覆盖区应用壤中气汞量测量研究活动断裂是一种新方法,它不仅能较准确地确定活动断裂的位置,还可以确定其产状,规模,活动性及相对强度,甚至可以作为确定断裂力学性质的参考,本文简棕了断裂带壤中气汞量测量的基本原理,并以长江三峡,长春,吉林等地利用该种方法研究活动断裂的成果为例,说明该项研究的效果及应用前景。 相似文献
923.
924.
Mobility of Al, Co, Cr, Cu, Fe, Mn, Ni and V in sulphide-bearing fine-grained sediments exposed to atmospheric O2: an experimental study 总被引:1,自引:0,他引:1
Mats Åström 《Environmental Geology》1998,36(3-4):219-226
The major aim was to increase our knowledge on the behaviour of Al, Co, Cr, Cu, Fe, Mn, Ni and V in sulphide-bearing fine-grained
sediments exposed to atmospheric oxygen. Samples of this type of sediment collected in a previous investigation at eight sites
in western Finland were digested in HClO4-HNO3-HCl-HF at 200 °C and in HCl:HNO3:H2O at 95 °C (aqua regia), and subjected to extractions with ammonium acetate and hydrogen peroxide. Metals and S in the leachates
were determined with ICP-AES. The results of the chemical analyses are compared with previously reported experimental data.
The concentrations of Al and Fe in the sulphide-bearing fine-grained sediments are about 7% and 5%, respectively. Of the trace
metals studied, Mn is most abundant followed in decreasing order by V>Cr>Ni>Cu>Co. On oxidation of the sediments, high proportions
of Co, Mn and Ni, intermediate proportions of Cu but low proportions of Fe, Al, Cr and V are released. The extent of the release
of a metal on oxidation is controlled either by (1) the level to which the pH of the sediments drops on oxidation (Al, Cu,
Cr, V), (2) the amount of the metal associated with easily reduced phases (metal sulphides) in the sediments (Ni, Co) or (3)
the sum of the amount associated with reduced phases and adsorbed on soil compounds (Mn). No control of the release of Fe
on oxidation of the sediments was identified. Based on the results of the study it is argued that artificial drainage and
the subsequent oxidation of sulphide-bearing sediments will result in extensive leaching of Co, Mn and Ni, moderate leaching
of Cu and limited leaching of Cr and V into drainages. The major elements, Fe and Al, have the potential to be mobilised and
leached in large amounts, though the proportions mobilised/leached will remain low. It is suggested that the identification
of sulphide-bearing sediments with a high potential of metal release should be based on determination of metals in easily
mobilised reduced compounds (dissolved e.g. in H2O2) and of the level to which the pH of the sediments drops on oxidation.
Received: 16 October 1997 · Accepted: 9 March 1998 相似文献
925.
As in other regions colonised from Europe within the last few centuries, Australia's vegetation and soils have been dramatically changed by clearing, cropping and grazing. In southeastern Australia, particularly on the Southern Tablelands, the impacts of European settlement are clearly manifested by channel incision. By using stratigraphic and documentary evidence, in conjunction with aerial photographs, sediment budgets for the post-settlement period have been constructed to define the fluxes and stores of sediment for each of the major geomorphic components of the 136 km2 catchment of Jerrabomberra Creek near Canberra. Using these budgets, and some plausible assumptions, it has been possible to approximate the history of both the sediment delivery ratio and sediment yield for this catchment. While the quantities estimated in this analysis are approximations, the trends through time are credible. Sediment yield increased rapidly to a peak after European settlement, and has returned to a level between the peak and the pre-European value. The delivery ratio has followed a similar trend. The most general conclusion to emerge is that in this landscape both the total sediment flux and the sediment yield of the catchment have been dominated by channel erosion. This result is contrary to the findings in many parts of the world where sheet and rill erosion dominates the fluxes. The soil conservation implication of these results is clear: to control off-site effects of erosion, the focus must be on the channels. 相似文献
926.
Lloyd R. Stark Brent D. Mishler D.Nicholas McLetchie 《Journal of Arid Environments》1998,40(4):401-416
The low elevation Mojave Desert cryptobiotic crust is dominated by the mossSyntrichia caninervis. In 16 populations of this moss, stem height and population were significantly associated with sex expression, with longer stems expressing sex more frequently and producing more perichaetia. The above-ground age of stems ranged up to 10 years, with a mean growth rate across populations of 0.36 mm year−1. The overall stem sex ratio, as a proportion of the total number of stems, was 0.30♀: 0♂: 0.70 non-expressing. The probability of expressing sex in a given season was 0.09. The absence of sexual reproduction (no sporophytes) and likely absence of the male sex from the area indicate that the non-expressing plants are female individuals. The slow growth rates, low rates of sex expression, absence of male plants, and absence of sexual reproduction in this crustal species may help explain why re-establishment of mosses on desert soils can take decades. 相似文献
927.
南京太平门地段雪松树年轮及其根土中化学元素含量的相关性研究 总被引:6,自引:0,他引:6
1994年在南京市太平门街道采集了五株雪松的年轮样及其根部土壤(黄棕壤pH=6.68),分别测定了Li、Al、P、K、Mn、Co、Cu、Zn、Cd、Ba和Pb等11种化学元素含量,实测结果验证了雪松年轮与其根部当年土壤中化学元素含量满足对数线性相关模式;lgC′(Z,t)=a(Z)+b(Z)lgC(Z,t)。根据年轮元素含量C(Z,t)可以重建过去根土中元素含量C′(Z,t),即反映环境(土壤)中元素含量的逐年演变的年份序列。利用C(Z,t)中最低含量可估算该地段黄棕壤的土壤元素背景值。 相似文献
928.
塔里木河流域绿洲边缘土壤蒸发与积盐的初步分析 总被引:8,自引:1,他引:7
本文通过对塔里木河流域土壤分的分析测定,视频研究了盐分积累的特点及其与蒸发的关系;盐分含量高,累积速度快、表聚性强。 相似文献
929.
陕西神府矿区束鸡沟流域风蚀水蚀交互作用特征研究 总被引:6,自引:1,他引:5
以神府矿区束鸡沟为典型小流域,讨论了风蚀水蚀交互作用的时空分布及其特征。风蚀水蚀交互作用在沙质坡面,坡面切沟和沙质沟道区表现最为突出,并形成了风蚀水蚀交互作用特有的侵蚀形态。 相似文献
930.
CAI Qiangguo 《国际泥沙研究》1998,(2)
PHYSICALPROCESSBASEDSOILEROSIONMODELINASMALLWATERSHEDINTHEHILLYLOESSREGION1CAIQiangguo2ABSTRACTAphysicalprocesbasedperstorm... 相似文献