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Kuang Wenhui Zhang Shuwen Du Guoming Yan Changzhen Wu Shixin Li Rendong Lu Dengsheng Pan Tao Ning Jing Guo Changqing Dong Jinwei Bao Yuhai Chi Wenfeng Dou Yinyin Hou Yali Yin Zherui Chang Liping Yang Jiuchun Xie Jiali Qiu Juan Zhang Hansong Zhang Yubo Yang Shiqi Sa Rigai Liu Jiyuan 《地理学报(英文版)》2022,32(9):1705-1723
Journal of Geographical Sciences - High-resolution mapping and monitoring of national land use/cover changes contribute significantly to the knowledge of the interaction between human activities... 相似文献
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André M van der Schaar M Zaugg S Houégnigan L Sánchez AM Castell JV 《Marine pollution bulletin》2011,63(1-4):18-26
The development and broad use of passive acoustic monitoring techniques have the potential to help assessing the large-scale influence of artificial noise on marine organisms and ecosystems. Deep-sea observatories have the potential to play a key role in understanding these recent acoustic changes. LIDO (Listening to the Deep Ocean Environment) is an international project that is allowing the real-time long-term monitoring of marine ambient noise as well as marine mammal sounds at cabled and standalone observatories. Here, we present the overall development of the project and the use of passive acoustic monitoring (PAM) techniques to provide the scientific community with real-time data at large spatial and temporal scales. Special attention is given to the extraction and identification of high frequency cetacean echolocation signals given the relevance of detecting target species, e.g. beaked whales, in mitigation processes, e.g. during military exercises. 相似文献
995.
Ke-Sheng Cheng Ju-Chen Hou Jun-Jih Liou Yii-Chen Wu Jie-Lun Chiang 《Stochastic Environmental Research and Risk Assessment (SERRA)》2011,25(2):107-122
A frequency-factor based approach for stochastic simulation of bivariate gamma distribution is proposed. The approach involves
generation of bivariate normal samples with a correlation coefficient consistent with the correlation coefficient of the corresponding
bivariate gamma samples. Then the bivariate normal samples are transformed to bivariate gamma samples using the well-known
general equation of hydrological frequency analysis. We demonstrate that the proposed bivariate gamma simulation approach
is capable of generating random sample pairs which not only have the desired marginal densities of component random variables
but also their correlation coefficient. Scatter plots of simulated bivariate sample pairs also exhibit appropriate linear
patterns (dependence structure) that are commonly observed in environmental and hydrological applications. Caution should
also be exercised when specifying combinations of coefficients of skewness and the correlation coefficient for bivariate gamma
simulation. 相似文献
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提出了一种拓扑关系和方向关系组合描述框架,在统一的框架下研究拓扑和方向关系。采用9交模型描述拓扑关系,方向关系矩阵模型表达方向关系,并给出了有意义的方向片组合,将两者统一到一个框架下进行描述。在统一描述框架下,拓扑关系与方向关系相互约束。阐述了7个定理及其证明,描述了拓扑关系与方向关系之间的相互约束,实现拓扑关系和方向关系有效性的相互检测。拓扑关系和方向关系组合描述能够提高空间关系描述的准确性和有效性。 相似文献
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The Gushan deposit is one of the typical magnetite–apatite deposits associated with dioritic porphyries in the Lower Yangtze River Valley belt of the eastern Yangtze craton. The origin of this deposit is still uncertain and remains a controversial issue. Divergent opinions are centered on whether the iron deposits are magmatic or hydrothermal in origin. However, our field observations and mineralogical studies, combined with previous published petrological and geochemical features strongly suggest that the main ore bodies in the Gushan magnetite–apatite deposit are magmatic. Specific evidence includes the existence of gas bubbles, tubes, and miarolitic and amygdaloidal structures, melt flow banding structure and the presence of “ore breccia”. New electron microprobe analyses of the pyroxene phenocrysts of the dioritic porphyry genetically associated with the Gushan magnetite–apatite deposit show that the Fe contents in the evolving magma dramatically decrease, and then gradually increase. Because there is no evidence of mafic magma recharge, this scenario (decreasing Fe) could be plausibly interpreted by Fe-rich melts separated from Fe-poor silicate melts, i.e., liquid immiscibility was triggered by minor addition of phosphorus by crustal contamination. The occurrence of massive iron ore bodies can be satisfactorily explained by the immiscible Fe-rich melt with enormous volatile contents was driven to the top of the magma chamber due to the low density. The hot and volatile-rich iron ore magma was injected along fractures and spaces between the dioritic intrusions and wall-rocks, and led to an explosion near the surface, resulting in the immediate fragmentation of the roof of the intrusion and wall-rocks, forming brecciated ores. Moreover, other types of ores can be considered as a result of post-magmatic hydrothermal activities. Our proposed metallogenic model involving the Kiruna-type mineralization is consistent with the observed phenomenon in the Gushan deposit. 相似文献
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