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31.
互花米草是中国东部河口滩涂湿地主要入侵物种之一,其与本地物种芦苇竞争生长,形成了大范围的混合交错带。该交错带是研究湿地生态系统动态变化的重要信息,但因2种物种光谱的相似性及其在交错带的组成复杂性,使利用遥感技术提取交错带难度较大。因此,本文提出了一种将二者生长物候差异与其光谱特征相结合,考虑二者海陆位置分布差异,运用实测剖面观测数据确定光谱指标和阈值的综合提取方法。运用高分一号多光谱遥感数据,通过分析不同时相互花米草与芦苇冠层光谱差异,确定用来提取混合交错带的高分遥感影像,实现了研究区互花米草-芦苇混合交错带的提取。结果表明:不同时相宜选用不同的提取指标,本研究中在春季选择了近红外波段反射率,而秋季则选择了红波段反射率;2个时相的混合交错带范围存在明显差异,客观反映了互花米草与芦苇在不同季节的竞争状况。  相似文献   
32.
为研究芦苇盐沼植物在一个生长周期不同生长季节的雷达后向散射系数变化特征,对芦苇分布信息进行提取,探究Sentinel-1A卫星数据在长江口湿地植被监测中的应用前景。以对长江河口崇明东滩南部为研究区域,利用2016年11个时相的Sentinel-1A雷达卫星影像VV(vertical transmit/vertical receive)+VH(vertical transmit/horizontal receive)双极化数据,分析潮滩地带芦苇、白茅、海三棱藨草、水体和光滩在植被生长周期内的雷达后向散射强度变化特征,对芦苇盐沼植被进行识别提取。结果表明:相较于VH极化方式,VV极化方式下不同地物的后向散射强度差异更为明显,芦苇的后向散射强度在枯叶期下显著高于其他地物;进行芦苇植被提取时,需要对植被枯萎期不同潮位状况下的雷达影像进行组合运算,芦苇提取精度可达到88.7%;对芦苇植被雷达后向散射强度和临近时相的光学遥感归一化植被指数(normalized difference vegetation index,INDV)进行相关性分析,发现两者呈良好的正相关关系,相关系数为0.78。  相似文献   
33.
科尔沁沙地典型生境下芦苇的生长特征分析   总被引:3,自引:3,他引:0  
对科尔沁沙地两类典型生境下芦苇根茎生长及生物量等特性进行了分析研究。结果表明,固定样地芦苇株高、分蘖株数、不定芽数、根茎节数及根茎总长均大于半流动样地。从半流动样地到固定样地,芦苇根茎表现出节间长度缩短,节间直径变粗的趋势。固定样地芦苇叶长、叶宽明显大于半流动样地,并且固定样地芦苇叶间距是半流动样地上的近3倍。与半流动样地相比,固定样地根茎生物量在总生物量中所占比例有所增加,而地上生物量所占比例减小。芦苇根茎生长及生物量分配在两类样地间的变化特征与土壤质地、紧实度以及养分含量等因素有密切的联系,同时也反映了芦苇对不同沙生生境的适应对策。  相似文献   
34.
闽江河口湿地芦苇和互花米草氮、磷养分季节动态   总被引:8,自引:0,他引:8  
于2007年对闽江河口湿地优势本地种芦苇(Phragmites australis)和外来入侵种互花米草(Spartina alterniflora)N、P养分含量与生物量进行1 a的观测.结果表明,两种植物地上部分N、P含量的器官分配模式为叶最高,花次之,茎最低,其中芦苇叶N含量显著高于互花米草(n=3,p<0.05);两种植物绿色部分N、P含量高于立枯部分;季节动态为冬、春季节高于夏、秋季节;N、P积累在不同器官的分布大致趋势为叶最高,茎次之,花最低,其中互花米草绿色茎和绿色叶N、P积累量显著高于芦苇(n=3,p<0.05);芦苇地下部分N、P含量变化趋势为0~15 cm最高,15~30 cm次之,30~60 cm最低,而互花米草与之相反;两种植物地下N、P积累量变化都为0~15 cm最高,15~30 cm次之,30~60 cm最低;芦苇地下部分N、P积累量在各个季节始终高于地上部分,但互花米草与之相反.从N/P看,N素为两种植物生产力的重要限制营养因子.  相似文献   
35.
Southern right whales (Eubalaena australis) were widespread in New Zealand waters before commercial whaling in the nineteenth century caused drastic declines in their abundance and distribution. Following the cessation of whaling, the population has been recovering and is now slowly recolonising its former range. Estimates of population demographics, including reproductive output, are essential for predicting the trajectory of this population. We gathered photo-identification data on female southern right whales during annual field trips to the Auckland Islands, the principal calving area in New Zealand waters. Forty-five calving intervals were observed between 2006 and 2013 (mean interval?=?3.31 years, 95% CI?=?3.06–3.57). Incorporating the effects of possible missed calving events produced a plausible range of mean calving intervals from 3.17 to 3.31 years. Our results suggest that the calving interval of New Zealand southern right whales is similar to that found in populations elsewhere.  相似文献   
36.
37.
太湖滨岸带芦苇区沉积物磷的特征   总被引:4,自引:0,他引:4  
为了进一步揭示大型水生植物对湖泊滨岸带沉积物磷的生物地球化学影响,探讨芦苇(Phragmites austra-lis)群落对沉积物磷的生态效应,于2003年9月18日、10月17日和12月3日,用柱状采样器分别在太湖梅梁湾滨岸带芦苇区和无草对照区采样。用HClO4-H2SO4消化法和H2SO4-H2O2消煮法测定芦苇区和对照区沉积物及芦苇根、茎组织中的总磷含量。结果表明,在芦苇生长旺盛期(9月),芦苇区和对照区沉积物的总磷含量最高,在芦苇生长的衰弱期(10月),其总磷含量次之,在芦苇生长的枯萎期(12月),其总磷含量最低;对照区沉积物距地表0~2cm的表层是磷的富集峰值层,而芦苇生长区距地表4~7cm的沉积物层为磷的富集峰值层;芦苇须根对磷的富集效应大于其根状茎,而芦苇根状茎对磷的富集效应又大于其茎,但它们的总磷含量都小于距根0~2cm范围芦苇根际沉积物的总磷含量。  相似文献   
38.
Partitioning evapotranspiration (ET) into evaporation (E) and transpiration (T) in wetlands is important for understanding the hydrological processes in wetlands and the contribution of wetland ET to local and regional water cycling and for designing effective wetland management strategies. Stable water isotopes are useful in the application of ET partitioning through the evaluation of the isotopic compositions of E (δE), T (δT), and ET (δET) obtained from observation or modelling methods. However, this approach still suffers from potentially large uncertainties in terms of estimating the isotopic endmembers. In this study, we modified the traditional isotope‐based ET partitioning methods to include leaf‐level biological constraints to separately estimate the relative contributions of T from Scirpus triqueter and Phragmites australis and the relative contributions of E from the standing surface water in a semiarid marsh wetland in northeastern China. The results showed that although the δT values of Striqueter and Paustralis were rather similar, the mean δT values of the 2 species were different from the values of δE, making it possible to distinguish the relative contributions of E and T through the use of isotopes. The simulation of leaf water using a non‐steady‐state model indicated obvious deviations in leaf water enrichment (δLb) from isotopic steady states for both species, especially during early mornings and evenings when relative humidity was highest. The isotopic mass balance showed that E accounted for approximately 60% of ET, and T from Striqueter and Paustralis each contributed approximately 20% to ET; this implied that the transpiration of one reed was equivalent to that of 5.25 individuals of Striqueter. Using the estimated ratio of T to ET and the measured leaf transpiration, the total ET was estimated to be approximately 10 mm day?1. Using the NSS‐Tr method, the estimated ET was higher than the water loss calculated from the water level gauge. This indicated that the river water and surrounding groundwater were the sources of the marsh wetland, with a supply rate of 8.3 mm day?1.  相似文献   
39.
Sediment and hydrodynamics of the Tauranga entrance to Tauranga harbour   总被引:2,自引:2,他引:0  
To relate the textural characteristics of the bottom sediments of a tidal inlet to hydrodynamics, 45 sediment samples from the Tauranga Entrance to Tauranga Harbour were analysed for textural parameters, and tidal currents and waves were monitored. Tidal currents dominate sediment transport processes near the Tauranga Entrance although swell waves are significant on the ebb tidal delta, and wind waves may influence intertidal sediments within the harbour. The bulk of the sediment is probably derived from marine sand from the Bay of Plenty continental shelf, but tidal currents and waves have changed its textural character. In areas of swift tidal currents, particularly in the inlet channel itself, sediment is coarser, more poorly sorted, and more coarsely skewed than that in areas of slower currents.  相似文献   
40.
Neocalanus tonsus, C. macrocarinatus, and C. australis, three calanids which potentially occur together in New Zealand waters, were raised from eggs and their developmental stages described. All naupliar stages apparently have identical setation. Naupliar stages I—III are very similar. Neocalanus tonsus can be easily identified from naupliar stage IV onwards, whereas C. macrocarinatus and C. australis can be identified with certainty only in the copepodite stages, because their nauplii overlap in size and body proportions. Development at 15 °C from egg to copepodite V took 24 days for N. tonsus, 20.2 days for C. macrocarinatus, and 23.8 days for C. australis. Neocalanus tonsus is the smallest species during early developmental stages but by copepodite III stage is larger than the other two species.  相似文献   
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