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江苏省1998年夏熟作物减产气象条件分析   总被引:4,自引:1,他引:3  
吴炳娟  黄毓华 《气象》1999,25(6):47-49
江苏省1998年夏熟作物严重减产,导致减产的主要原因是气候异常,期间出现了罕见的全省性、全程性的涝渍害及冻、病等灾害,危害程度高,不可抗拒。作者对江苏省1998年夏熟作物减产的气象条件作出分析。  相似文献   
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在地震现场应急通信中,为满足无线图传系统等通信设备在复杂地形进行大范围和远距离通信作业的需求,提出利用系留式无人机中继通信系统保障无线电(超短波)的远距离传输。目前,对该系统的研究还处于理论分析和试验阶段,尚未在地震应急中得到大范围的推广应用。本研究利用多次试验的数据,分析验证系留式无人机供电系统的可行性及实用性,定量计算中继通信系统的升空效益,并形成一套完整的、可操作性强的系统实施方案。在城区、郊区以及起伏较低的山地、丘陵等地区,实现了移动图传系统在距离通信车5—10km范围内稳定、实时、快速的数据传输。  相似文献   
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宜兴太湖防护林对农业面源污染的减源增汇作用浅析   总被引:1,自引:1,他引:0  
为探讨太湖沿岸防护林宜兴段对农业面源污染物的控制效果,通过在宜兴市太湖防护林采集土壤样品,测定其中营养元素含量,结合周边农业生产施肥概况,初步分析了该区域防护林对农业面源污染的减源—增汇效应.结果表明,2009年10月份防护林地上部分固定的C、N、P和K分别为2439.48、18.34、2.48和13.42 g/m2;2011年5月份固定量分别为3114.12、23.42、3.16和17.13 g/m2;而2013年8月份固定量分别为4722.46、35.53、4.81和25.99 g/m2.可见C、N、P和K的固定量是逐年增加的,相比2009年,分别增加了93.6%、93.7%、94.0%和93.7%.结果说明宜兴段太湖沿岸防护林对农业面源污染的控制效果较显著,有助于太湖水污染的治理.  相似文献   
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大亚湾核电站邻近水域桡足幼体现场摄食研究   总被引:1,自引:0,他引:1  
桡足类种类多、数量大、分布广, 在食物链中处于中间环节, 对海洋生态系统的结构稳定起着重要作用。桡足类幼体获取的营养直接影响其发育, 进而影响桡足类成体补充乃至种群的稳定。本研究于2015年夏季分别在大亚湾核电站邻近海域S1 (进水口水域)和S2 (排水口水域)站进行了调查采样, 应用分子生物学方法检测了桡足幼体现场摄食食物组成。结果显示: 1)两个站的桡足幼体内共检测到16种不同食物, 包括浮游植物(硅藻)11种, 后生动物2种、真菌、Ichthyosporea 和卵菌类各1种共5大类, 其中硅藻(47.30%, 克隆数百分比, 下同)和被囊动物类后生动物(41.89%)是其主要的食物类群; 2)在S1和S2站桡足幼体内分别检测到9种和10种食物, 但主要食物类型有差异, S1站较多后生动物(61.54%), 而S2站较多硅藻(68.57%); 3) S2站的桡足幼体杂食偏植食程度更高, 其杂食性系数(0.31)低于S1站(0.72)。结果表明, 桡足幼体能根据食物环境有选择地摄食植物饵料和动物饵料, 调节食物营养结构; 温排水影响水域桡足幼体更偏向植食性, 尤其是硅藻, 暗示全球变暖可能导致桡足幼体食性偏移。  相似文献   
68.
利用日本东京大学气候系统研究中心、日本环境研究所和日本地球环境研究中心联合研制的全球海气耦合气候系统模式(MIROC_Hires)输出的逐日降水资料,探讨CO2浓度增加下我国极端降水非均匀性的响应及其可能机制。结果表明:(1)就气候平均而言,CO2浓度增加后,我国南部地区极端降水事件的发生更为集中,而北方地区的极端降水事件分布较平均。(2)从年际变率来看,我国南部地区极端降水事件集中度在"A1B试验"中偏小,年际之间的差异不大,而北方地区的极端降水集中度增加,年际之间变化剧烈。(3)CO2浓度增加后,南方和北方地区在水平和垂直上的增温幅度不一致,且整层大气平均的稳定度呈现出南北反相差异。这种不均匀增暖的分布很可能是导致我国极端降水非均匀性在CO2浓度增加后变化的原因。  相似文献   
69.
Forest harvesting often increases catchment quickflow (QF, water delivered rapidly to the stream channel), a metric of high‐flow events controlling a catchment's solute and sediment export. Nevertheless, our understanding of QF responses to various silvicultural strategies (e.g., clearcutting, selection harvest, and shelterwood harvest) is incomplete. We present a 31‐year examination of QF delivery from treatment (clearcut, selection harvest, and shelterwood harvest) and control catchments in a deciduous forest landscape in central Ontario, Canada. Growing season root‐zone storage capacity was estimated using a water balance approach to evaluate temporal changes in QF response to precipitation (P) for pretreatment and posttreatment periods. Threshold relationships between QF and P were assessed for control and treatment catchments for pretreatment and posttreatment periods using piecewise regression. Root‐zone storage capacity demarcated shifts in the hydrologic regime arising from forest harvesting and subsequent regeneration. This was particularly pronounced for clearcutting where postharvest decline in root‐zone storage capacity was followed by a rise to preharvest values. Similar pretreatment threshold relationships between QF and P, and near‐identical P thresholds for producing significant QF, reflected similar soil and overburden depths in the catchments. Harvesting effects were indicated by increases in QF/P ratios for relative small P and the number of P events that generated QF, thus changing treatment QF vs. P threshold relationships. Prior to harvesting there was no significant increase in QF with P below a threshold P of 35–45 mm; however, there was a significant QF vs. P relationship below this threshold for all treatments postharvest. Clearcutting increased the number of QF events for the entire postharvest period and the first 9‐year postharvest compared to the other treatments; nevertheless, evidence for intertreatment differences in total QF depth delivered from the catchments during the growing season was inconclusive. Our work suggests that changes in threshold relationships between QF and P, coupled with knowledge of the physical processes underlying them, are useful when evaluating hydrologic responses to forest harvesting.  相似文献   
70.
Headwater forest ecosystems of the western USA generate a large portion of the dissolved organic matter (DOM) transported in streams across North America. Land cover changes that alter forest structure and species composition affect the quantity and composition of DOM transferred to aquatic ecosystems. Clear-cut harvesting affects ~1% of the forest area of North America annually, leaving most western forests in varying stages of regrowth and the total area of old-growth forest is decreasing. The consequences of this widespread management practice on watershed carbon cycling remain unknown. We investigated the role of land cover change, because of clear-cut harvesting, from mixed-species old-growth to lodgepole pine-dominated second-growth forest on the character and reactivity of hillslope DOM exports. We evaluated inputs of DOM from litter leachates and export of DOM collected at the base of trenched hillslopes during a 3-year period (2016–2018) at the Fraser Experimental Forest in north-central Colorado, USA. Dissolved organic carbon and total dissolved nitrogen were higher in lateral subsurface flow draining old- versus second-growth forest. Fluorescence spectroscopy showed that the DOM exported from the old-growth forest was more heterogeneous and aromatic and that proteinaceous, microbially processed DOM components were more prevalent in the second-growth forest. Biological oxygen demand assays revealed much lower microbial metabolism of DOM in litter leachate and subsurface exports from the old-growth forest relative to second growth. Old-growth and second-growth forests are co-mingled in managed ecosystems, and our findings demonstrate that land cover change from a mixture of conifer species to lodgepole pine dominance influences DOM inputs that can increase the reactivity of DOM transferred from terrestrial to aquatic ecosystems.  相似文献   
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