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991.
自2018年12月起,因洛阳地震台测区内安装金属护栏,该台地电阻率出现异常变化。为正确评估此次影响,结合洛阳地震台电测深曲线、岩性资料建立了三维水平层状结构模型,利用有限元法计算了测区内金属护栏对洛阳地震台地电阻率观测的影响。同时,建立典型“H”型电性结构模型,分析了不同属性的金属导线对地电阻率观测的影响。结果显示:①金属护栏是洛阳地震台此次地电阻率年变异常的主要影响因素。当位于测区内影响系数为负的区域时,金属护栏引起地电阻率的趋势性上升;当位于影响系数为正的区域时,金属护栏引起地电阻率的趋势性下降。②不同属性的金属导线对地电阻率观测的影响不同。导线与测道夹角减小、导线长度增加、导线电阻率减小以及导线横截面积增加等均会导致干扰源对地电阻率年变影响作用增强。 相似文献
992.
以广州市人民公园为研究对象,通过实地踏勘和问卷调查,利用统计与观察分析方法解剖城市公园游憩行为的性别差异特征。在游憩者的行为和社会特征方面,两性之间存在明显差异;女性的公园游憩行为与其社会分工特别是家庭责任紧密联系;女性因对安全性的要求高而趋向视线开敞的集体区域活动,男性因要求独立性而趋向在有视线遮挡的区域活动,且男性同性恋活动区域对女性形成了一定的活动抑制;女性对出行距离较为敏感,而男性独自出行游憩的比例更高;女性对城市游憩空间的需求趋于稳定、有规律,也凸显了公园对女性日常生活的重要性。基于公平性与人性化原则提出相应的城市公园规划设计对策,特别应对公共设施进行细致而灵活的设计,以适应使用者的性别差异性;并应按照步行尺度进行游憩场所的规划布局,以保障女性就近游憩的需求。 相似文献
993.
Suspended sediment load in the turbidity maximum zone at the Yangtze River Estuary:The trends and causes简 总被引:6,自引:2,他引:4
Based on the analysis of suspended sediment elements at estuaries, influence of human activities and estuarine regulation projects on the turbidity maximum zone was studied according to the measurement data between 1959 and 2011. It was found that human activi- ties had little effect on the seaward water while the sharp decrease of sediment volume and concentration in runoff led to the sharp decrease of turbidity maximum zone in the estuary. The concentration at outside sea and Hangzhou Bay did not change, and that along the Subei coast also decreased a little, which had no influence on the turbidity maximum zone. Com- pared with the concentration between 1959 and 1999, the peak of concentration moved up- stream in the estuary, and the concentration in 2000-2009 decreased by about 24.73% with a narrower variation range along the river to the sea. The suspended sediment concentration in North Passage was low in upstream and downstream because of the decrease of seaward sediment and coarsening of bed material, while it was relatively high in the middle due to the influence of sediment cross the north jetty. 相似文献
994.
995.
Variation of particulate organic carbon and its relationship with bio-optical properties during a phytoplankton bloom in the Pearl River estuary 总被引:2,自引:0,他引:2
Wang G Zhou W Cao W Yin J Yang Y Sun Z Zhang Y Zhao J 《Marine pollution bulletin》2011,62(9):1939-1947
In this study, variations in the particulate organic carbon (POC) were monitored during a phytoplankton bloom event, and the corresponding changes in bio-optical properties were tracked at one station (114.29°E, 22.06°N) located in the Pearl River estuary. A greater than 10-fold increase in POC (112.29-1173.36 mg m−3) was observed during the bloom, with the chlorophyll a concentration (Chl-a) varying from 0.984 to 25.941 mg m−3. A power law function is used to describe the relationship between POC and Chl-a, and the POC:Chl-a ratio tends to change inversely with Chl-a. Phytoplankton carbon concentration is indirectly estimated using the conceptual model proposed by Sathyendranath et al. (2009), and this carbon is found to contribute 47.21% (±10.65%) to total POC. The estimated carbon-to-chlorophyll ratio of phytoplankton in diatom-dominated waters is found to be comparable with results reported in the literature. Empirical algorithms for determining the concentrations of Chl-a and POC were developed based on the relationships of these variables with the blue-to-green reflectance ratio. With these bio-optical models, the levels of particulate organic carbon and Chl-a could be predicted from the radiometric data measured by a marine optical buoy, which showed much more detailed information about the variability in biogeochemical parameters during this bloom event. 相似文献
996.
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
997.
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
998.
999.
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
1000.