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301.
基于主客观赋权模糊综合评价法的湖泊水生态系统健康评价 总被引:2,自引:0,他引:2
运用湖泊营养状态指数判断湖泊的富营养化状态,并根据湖泊的水质、沉积物和水生生物群落的现状和特点,运用主观赋权法中的层次分析法和客观赋权法中的熵权法结合模糊综合评价法,对长江中游地区江汉湖群37个湖泊的水生态系统进行健康状态评价.对湖泊富营养化的调查结果表明,海口湖处于中营养状态,18个湖泊处于富营养化状态,18个湖泊处于超富营养化状态.湖泊生态系统健康评价的研究结果表明,37个湖泊中,处于健康状况"优"的湖泊只有海口湖,处于健康状况"良"的湖泊有5个,分别为东西汊湖、花马湖、梁子湖、童家湖和涨渡湖,其余31个湖泊均处于健康状况"差"的状态.经过与湖泊营养状态指数的对照,本研究结果表明,由主观赋权的专家评分的层次分析法结合模糊综合评价法对江汉湖群湖泊水生态健康状态的评价效果相比客观赋权的熵权模糊综合评价法更贴合实际. 相似文献
302.
ZHANG Yan-hui LI Shi-wen WENG Ai-hua ZHANG Su-qin YANG Yue LI Jian-ping TANG Yu 《地震地质》2019,41(4):979-995
Geomagnetic depth sounding is an effective method for exploring deep structure of the earth. There are dense geomagnetic observatories in China, which lays a foundation to obtain the electrical structure of the transition zone and the upper part of the lower mantle beneath China. However, the corresponding C-responses estimation methods which are applied now cannot get the stable C-responses for many observatories. Thus, a large amount of geomagnetic data is wasted. Therefore, in order to make full use of the geomagnetic data, the estimation of C-responses needs to be systematically studied. Because of the heterogeneous characteristics of the data quality of China's geomagnetic observation data, such as the quality of the data, the length of the record, the types of data(absolute and relative observation)and data discontinuity condition, many geomagnetic data are abandoned, this limits the resolution of mantle electrical structure studies. In this paper, the following techniques are used to improve the stability of the data and increase the number of the available geomagnetic observatories, in the meantime, the stability of the C-responses curves can be effectively improved:1)obtaining the stable spectrums of the different components for each frequency by the BIRRP(Bounded Influence, Remote Reference Processing)software, and using the global smoothing technique to suppress data noise on geomagnetic data; 2)As for the geomagnetic data which only records the relative variation of the D, H and Z components and doesn't have the baseline value, the horizontal component is decomposed by the approximate estimation method to obtain the C-responses of the relative variation data, and then the relative variation data is used directly for the C-responses estimation; 3)the effects of discontinuous data and short-record data on C-responses estimation are discussed. Under normal conditions, the discontinuity of the data has little influence on C-responses, and when the data length is shorter than 5 years, we can hardly get the available C-responses whose periods are longer than 40 days. All these experiments can provide a basis for the data processing of these kinds of observation data; 4)for coastal observatories, the ratio method is used to eliminate the influence of ocean effect on the C-responses functions. After carefully processing the data of more than 100 geomagnetic observatories in China by the above techniques, the stable C-responses function of 42 observatories is finally obtained, among them, the number of the observatories with C-responses ranging from 1.3 to 113.7 days is 24, and the observatories with C-responses ranging from 1.3 to 42.6 days are 18. The techniques of this paper can process heterogeneous data well and obtain more stable C-responses, which provides more basic data for high-resolution geomagnetic depth sounding inversion researches in China. 相似文献
303.
叠前地质统计学反演将随机模拟与叠前反演相结合,不仅可以反演各种储层弹性参数,还提高了反演结果的分辨率.基于联合概率分布的直接序贯协模拟方法可以在原始数据域对数据进行模拟,不需要对数据进行高斯变换,拓展了地质统计学反演的应用范围;而联合概率分布的应用确保了反演参数之间相关性,提高了反演的精度.本文将基于联合概率分布的直接序贯协模拟方法与蒙特卡洛抽样算法相结合,参考全局随机反演策略,提出了基于蒙特卡洛优化算法的全局迭代地质统计学反演方法.为了提高反演的稳定性,我们修改了局部相关系数的计算公式,提出了一种新的基于目标函数的优化局部相关系数计算公式并应用到协模拟之中.模型测试及实际数据应用表明,该方法可以很好的应用于叠前反演之中. 相似文献
304.
FINE ELECTRICAL STRUCTURE BENEATH THE EPICENTER OF 1668 TANCHENG MS8.5 EARTHQUAKE REVEALED BY MT SOUNDING 下载免费PDF全文
WENG Ai-hua LI Jian-ping FAN Xiao-ping LI Si-rui HAN Jiang-tao LI Da-jun LI Ya-bin ZHAO Xiang-yang TANG Yu 《地震地质》2018,40(2):396-409
In order to understand the mechanism of the 1668 MS8.5 earthquake occurred in Tancheng, it is important to probe the fine deep geological structure beneath the epicenter. A MT profile 20km south of the epicenter has been deployed. There are 17 sites along the profile, with a 3km average separation. Signals in Ex, Ey, Hx and Hy were measured in a cross manner, with x-axis orientated to the north. Record length for each site was at least 20h. The impedance and phase at sites in high cultural noisy environment were estimated by remote reference technique. As the Tanlu Fault Zone(TLFZ)is in NNE, nearly northerly, thus YX mode was considered as TM mode. Gauss-Newton inversion was done in 2-D mode with only the TM impedance and phase as input data. The electrical sections of 10km and 40km depth were respectively obtained after 8 iterations. The both initial models were created by Bostic approximation. The sections reveal the following features.
The TLFZ consists of five faults, from east to west numbered as F0 to F4. F1 is the primary fault, steeply dipping west down to mantle, which has turned into a buried one overthrust by the east dipping Fault F0. F2 and F3 dip east at 45 degrees, parallel to F4, truncated by F1 at depth. F4 dips east in the shallow subsurface and gradually dips to west toward depth through the entire crust merging with F1 to form a bigger one. These four faults constitute a flower-shaped structure, showing the nature of strike-slip of the TLFZ, associated with normal faulting in the late Yanshanian to early Himalayan. F1 dips west, overthrust by east-dipping F0, implying the compression from the westward subduction of the Pacific plate, thus present-day compression is superposed on the early tensile and strike-slip feature.
Based on MT data, it is inferred that the 1668 Tancheng M8.5 earthquake occurred at the junction of F1 and F3 about 15km deep. Thus it was likely resulted from westward compression of the Pacific plate, leading to thrust of the Sulu uplift along F0, inducing activity of F1 at depth, reactivated F3, and adjusting the stress distribution in the region. 相似文献
305.
几次大地震前后地电场中长期变化分析与研究 总被引:1,自引:0,他引:1
地电场是地球表面天然存在的电场, 包括大地电场和自然电场。 利用“合成能量累加”方法, 分析处理了甘肃省、 青海省、 四川省、 重庆市所辖部分台站2007年7月至2017年12月的地电场观测数据, 研究和讨论了汶川8.0级地震等几次大地震前后地电场中长期异常变化特征。 研究结果显示, 几次MS7.0以上大地震前后, 均出现了地电场区域性准同步异常变化; 地电场异常变化经历了“震前—发震—震后”三个阶段, 震前和震后变化比较明显, 发震期变化相对平稳, 时间跨度达12个月以上; 地电场异常变化主要沿构造带分布, 变化强度随震中距的增加而减小。 相似文献
306.
GB-SAR变形监测技术研究现状与展望 总被引:1,自引:0,他引:1
地基合成孔径雷达(GB-SAR)技术是近十多年发展起来的地面主动微波遥感技术,可进行非接触、高精度、大范围、远距离的变形监测,在变形监测领域具有重要意义。本文首先介绍了GB-SAR干涉测量基础理论和研究现状,归纳了目前主要的GB-SAR系统,详细列举了现有系统的关键参数;进而分析了GB-SAR技术在基础设施、滑坡、矿山、冰川运动及文物保护等变形监测领域应用的优势和不足,总结了地基雷达系统在实际应用中面临的挑战;最后从多维形变、大气改正等方面对其应用前景进行了展望。 相似文献
307.
Antioxidant systems are vital in life activities of macrophytes. Species with dif ferent life forms need to cope with distinct environments by modifying physiological characters, especially antioxidant systems. In order to find dif ferences among life forms and consequence of lake eutrophication, we studied three antioxidant enzymes activity(superoxide dismutase(SOD), ascorbate oxidase(APX) and catalase(CAT)) and total soluble phenolics(TP) content in leaves of 26 macrophyte species in September 2013 in Lake Erhai, China. We found that antioxidation varied accordingly with life forms. The activities of SOD and APX in emergent macrophytes(EM) and floating-leaved macrophytes(FM) were much lower than those of submerged macrophytes(SM). On the contrary, TP content was much higher in EM and FM species. There was a negative correlation between TP and antioxidant enzyme activities(CAT and APX).The results suggested that EM and FM species rely on phenolics might to adapt to adverse environments(higher herbivores predation pressure and UV radiation intensity), while SM species more rely on antioxidant enzymes possibly due to lower demand for antioxidation and/or lack of light and inorganic C availability for phenolics synthesis. We also found FM species represent highest fitness in term of antioxidant system,which would lead to overgrowth of FM species and littoral zone bogginess during lake eutrophication.Finally, it is necessary to carry out the verification experiment under the control condition in the later stage,especially for the dominant ones in eutrophic lakes, to understand the exact adaptive mechanisms of them. 相似文献
308.
评估以多路径效应为代表的次周日周期信号对短基线时间序列的影响,结果表明,多路径效应在序列高程方向上引入0.1~0.3 mm虚假长周期信号,而对平面方向的贡献不大;与高度角有关的未模型化的次周日信号在单日解时间序列高程方向引入的虚假长周期信号不可忽略,适当提高截止高度角可予以减弱。 相似文献
309.
310.