全文获取类型
收费全文 | 7556篇 |
免费 | 1088篇 |
国内免费 | 989篇 |
专业分类
测绘学 | 682篇 |
大气科学 | 1068篇 |
地球物理 | 2371篇 |
地质学 | 3485篇 |
海洋学 | 785篇 |
天文学 | 373篇 |
综合类 | 300篇 |
自然地理 | 569篇 |
出版年
2024年 | 14篇 |
2023年 | 63篇 |
2022年 | 158篇 |
2021年 | 201篇 |
2020年 | 131篇 |
2019年 | 172篇 |
2018年 | 559篇 |
2017年 | 510篇 |
2016年 | 398篇 |
2015年 | 308篇 |
2014年 | 234篇 |
2013年 | 326篇 |
2012年 | 851篇 |
2011年 | 623篇 |
2010年 | 321篇 |
2009年 | 352篇 |
2008年 | 338篇 |
2007年 | 302篇 |
2006年 | 318篇 |
2005年 | 981篇 |
2004年 | 981篇 |
2003年 | 741篇 |
2002年 | 265篇 |
2001年 | 156篇 |
2000年 | 116篇 |
1999年 | 52篇 |
1998年 | 16篇 |
1997年 | 23篇 |
1996年 | 11篇 |
1995年 | 4篇 |
1994年 | 6篇 |
1992年 | 3篇 |
1991年 | 11篇 |
1990年 | 11篇 |
1989年 | 5篇 |
1987年 | 4篇 |
1986年 | 6篇 |
1983年 | 4篇 |
1980年 | 3篇 |
1979年 | 3篇 |
1977年 | 3篇 |
1976年 | 5篇 |
1975年 | 4篇 |
1965年 | 4篇 |
1961年 | 2篇 |
1959年 | 2篇 |
1955年 | 2篇 |
1954年 | 5篇 |
1951年 | 2篇 |
1948年 | 2篇 |
排序方式: 共有9633条查询结果,搜索用时 234 毫秒
1.
采用室内实验生态学方法,以水体中氨氮、活性磷酸盐和溶氧变化为指标研究了光照强度和光色对番红砗磲代谢的影响。结果表明:(1)在0—10000lx光照时,番红砗磲排氨量逐渐减少,在光照12000lx时转为吸收海水中氨氮,并在16000lx时达到最高[1.89μg/(ind·h)];在2000lx光照条件下,番红砗磲可吸收海水中活性磷酸盐并释放氧气。其活性磷酸盐吸收量随光照强度增强而增加,在16000lx时达到最高峰。在实验光照范围内,番红砗磲产氧率随光照强度的增强逐渐增加。上述结果显示番红砗磲最佳光照强度约为16000lx。(2)当番红砗磲自黑暗转移至各光照组后,其氨氮、活性磷酸盐吸收率均随时间逐渐降低,而产氧率则逐渐升高。(3)光色显著影响番红砗磲合成代谢,蓝光最佳,红光次之,白光最差。 相似文献
2.
似刺鳊鮈肌肉营养成分与品质的评价 总被引:1,自引:0,他引:1
利用常规方法对似刺鳊鮈(Paracanthobrama guichenoti Bleeker)进行了含肉率、可食率、肌肉弹性、肌肉营养成分测定并系统评价了鱼肉品质,旨在评价似刺鳊鮈的营养价值,为似刺鳊鮈的营养生理、养殖和加工研究提供基础资料.结果显示,似刺鳊鮈雄鱼的含肉率为(72.76±0.89)%,雌鱼为(68.99±0.76)%;雄鱼可食率为(78.36±0.93)%,雌鱼为(83.75±1.01)%;肌肉弹性值为(547.86±21.48)g;鲜样中粗蛋白含量为(18.10±0.17)%,粗脂肪含量为(2.32±0.13)%,水分(78.10±0.87)%,灰分(1.07±0.12)%;肌肉含有17种氨基酸,总量占鲜样的(14.91±0.31)%,其中7种人体必需氨基酸(除色氨酸外)含量占鲜样的(6.07±0.07)%,与非必需氨基酸的比值(EAA/NEAA)为68.67%,其必需氨基酸构成比例基本符合FAO/WHO的标准.必需氨基酸指数(EAAI)为73.46,支链氨基酸与芳香族氨基酸的比值(F值)为2.21,4种鲜味氨基酸占鲜样的5.73%;脂肪酸中EPA与DHA质量分数分别为2.94%,1.26%;微量元素含量丰富,钙镁含量较高;鱼肉品质系统评价结果表明,似刺鳊鮈是一种营养价值较高且有一定保健作用的鱼类. 相似文献
3.
4.
WiththedevelopmentofagricultureandChina'sentryintoWTO,thesituationofsupplyanddemandinmaizemarkethaschangedgreatly.Facingtherelativesurplusofmaizeandtheformationofbuyer'smarket,weshouldfullydeveloprelativeadvantages,carryouttheunevenstrategyofsupportingthesuperior inmaizeproduction andcultivateadvantagedareasofmaize.Theabovestrategicmeasurescanrapidlyim-provetheinternationally competitiveabilityandpro-ductivityofmaizeinJilinProvince,getoutofthea-griculturalpredicamentandmaketheagriculturalde-… 相似文献
5.
山东是饮用天然矿泉水资源大省 ,点之多、量之丰居全国前列。到目前为止 ,已鉴定矿泉水 36 1处 ,其中锶型118处 ,偏硅酸型 6 4处 ,锶偏硅酸型 15 1处 ,碘型等其它类型 2 8处。这些矿泉水所赋存的岩石类型多、岩性复杂且受断裂构造控制明显 ;具有达标元素较单一、水化学类型复杂、矿化程度较低、单井允许开采量相差悬殊且地域分布不均等特点。勘查与评价重点是寻找奇缺且又可能存在的锌型、锂型、碳酸型矿泉水。开发好矿泉水资源、实行规模开发、打造本省名牌、加强矿泉水资源的卫生防护与保护 ,对于确保山东矿泉水资源的持续开发与利用具有重要意义。 相似文献
6.
A component (s-factor) with obvious promoting effect on hydrogen evolution of hydrogenase has beenisolated and extracted from a Cell=free preparation of Spirulina platensis.The effect of the s-factor in the re-action system is similar to that of Na_2S_2O_4, but is coupled with ligh. The s-factor has the maximumabsorption peak at 620 nm in the oxidized state, at 590 nm in the reduced state. The partially purifieds-factor showed two bands by SDS-PAGE and is distinctly different from phycocyanin,which has nochange of oxidized state and reduced state absorption spectra, and also has no promoting effect onhydrogenase of Spirulina platensis under the light. 相似文献
7.
An Example of Island-Arc Petrogenesis: Geochemistry and Petrology of the Southern Luzon Arc, Philippines 总被引:7,自引:1,他引:6
DEFANT MARC J.; MAURY REN? C.; RIPLEY EDWARD M.; FEIGENSON MARK D.; JACQUES DARIO 《Journal of Petrology》1991,32(3):455-500
Volcanism throughout the Luzon arc is associated with eastwardsubduction of the South China Sea floor along the Manila Trench.The southern section of the arc, the focus of this study, extendsfrom the Lingayen-Dingalan fault to the small islands just southof Luzon. Two segments appear to exist along this section ofthe arc the northern Bataan and southern Mindoro segments whichare separated by the Macolod Corridor. The volcanic rocks have typical arc phenocryst mineralogies:olivine, clinopyroxene, plagioclase, and titanomagnetite inthe most mafic rocks and clinopyroxene, plagioclase, orthopyroxene,titanomagnetite, ? amphibole in the more felsic samples. Complexzoning, sieve textures, and decoupling of incompatible traceelements suggest that processes such as assimilation have takenplace. The rocks from the study area range from basalts to rhyolitesand show typical calc-alkaline features. The rocks of the MacolodCorridor and Mindoro segment are particularly enriched in largeion lithophile elements (LILE), light rare earth elements (LREE),and radiogenic Sr compared with the Bataan segment. The datafall within the mantle array on Sr-Nd isotopic diagrams andgrade toward higher Sr and lower Nd isotopic values from northto south. A likely source for the volcanics of this study is either amid-ocean ridge basalt (MORB)-type mantle that undergoes higherdegrees of partial melting than regions involved in MORB generationor a previously depleted source. We suggest that the high fieldstrength element (HFSE) anomalies have been derived throughdifferential element partitioning during fluid transport fromthe subducted lithosphere to the mantle wedge. Continental crustal material seems to play a significant roleparticularly in the Macolod Corridor and the Mindoro segment,based on the high LILE, La/Sm ratios, radiogenic Sr isotopes,and 18O values. The Macolod Corridor and the Mindoro segmenthave undergone source contamination by crustal material fromthe North Palawan-Mindoro crustal block either during the collisionof this block with the Manila Trench or by subduction of sedimentsrich in this crustal material. A similar component has alsobeen detected in the Bataan segment but in minor amounts. Thetrace element and isotopic differences between the northernand southern sections of the arc are interpreted in terms ofvariable composition (i. e., variable amounts of a crustal componentintroduced from the Palawan-Mindoro crustal terrain) of themetasomatic fluids released into the source. 相似文献
8.
Unconsolidated sand, gravel and clay deposits near Beihai and in the Leizhou Peninsula in southern China form an unconfined
aquifer, aquitard and a confined aquifer. Water and soil samples were collected from the two aquifers in the coastal Beihai
area for the determination of chemical compositions, minerals and soluble ions. Hydrogeochemical modeling of three flow paths
through the aquitard are carried out using PHREEQC to determine water–rock interactions along the flow paths. The results
indicate that the dissolution of anorthite, fluorite, halite, rhodochrosite and CO2, and precipitation of potash feldspar and kaolinite may be occurring when groundwater leaks through the aquitard from the
unconfined aquifer to the confined aquifer. Cation exchanges between Na and Ca can also happen along the flow paths. 相似文献
9.
10.
东天山黄山-镜儿泉过铝花岗岩矿物学、地球化学及年代学研究 总被引:3,自引:0,他引:3
对东天山黄山-镜儿泉一带黄山南、镜儿泉、图拉尔根沟三个过铝花岗岩作了岩相学、矿物学、地球化学、sr-Nd同位素和锆石U-Pb年代学研究.锆石U-Pb LA-ICP-MS原位定年测得黄山南岩体结晶年龄为259.9±1.4Ma(MSWD=0.86),图拉尔根沟岩体结晶年龄为275.4±8.3Ma(MSWD=29),均侵位于二叠纪碰撞后伸展环境.三个过铝花岗岩均具有低锶同位素初始比值(Isr=0.6969~0.70396)、高εNd(t)值( 5.5~ 7.2)以及年轻的亏损地幔单阶段模式年龄(tDM=0.48~0.56Ga),表明其岩浆源区均为来源于亏损地幔的新生地壳岩石.这种新生地壳岩石可能为偏酸性的火山岩.三个岩体的矿物学和地球化学可分为两类:一类以黄山南白云母花岗岩为代表,为强过铝花岗岩(A/CNK>1.1),强烈亏损Ba、sr和Ti而富集Cs、Rb和K,具有高的Rb/sr(2.03~14.5)和Al2O3/TiO2(110~1592),低的Nb/Ta(3.24~6.76)比值,其稀土元素配分曲线呈"V"字形,显示强烈铕亏损(Eu/Eu*=0.04~0.55),表明这类岩体的直接源岩以泥质岩为主.另一类以图拉尔根沟二云母花岗岩为代表,为弱过铝(1相似文献