小波分析在声发射资料处理中的初步应用   总被引：1，自引：0，他引：1  

陈顺云  杨润海  王赟赟  赵晋明  许昭永 《地震研究》2002,25(4):328-334

针对声发射数据分析的一些难点，把最近20年发展起来的小波技术引入声发射资料处理中，分析证明结果可靠。它在本中的应用有：（1）提取有效信息。小波强大分解（细化0能力可用来从高口音中找出有效记录，分解合成时可以去掉不理想的通道，使声发射数据更加“规则化”，有望实现到时自动判读。（2）对相互叠加的事件进行有效分离。结合全波记录，可使事件尽可能少丢失，提高声发射数量统计及b值计算等的精度。（3）使成份复杂的声发射波形数据分离成具有单一特征的波，但分解后的波究竟属于P波还是S波，甚至面波，尚难确定。  相似文献   

前驱地震波的试验研究及波谱分析   总被引：5，自引：1，他引：5  

王赟赟  杨润海  赵晋明  许昭永 《地震研究》2003,26(1):50-56

研究了含预置裂纹的有机玻璃试样在加载实验过程中，大破裂之前出现的长周期、小振幅低频事件，并与大地震前可能出现的同类现象（即前驱地震波）进行了对比研究，根据波形记录和频谱分析得出：前驱地震波是地壳介质的长周期波动，是一种客观存在的前兆特征，具有短临前兆意义。  相似文献   

重庆石碗溪小流域坡度和高程对土地利用及经济发展的影响   总被引：21，自引：3，他引：21  

罗云云  李瑞雪  屈明 《山地学报》2004,22(2):254-258

坡度和高程是土地资源固有的两个重要环境因子,与土地利用关系密切,尤其是在山区,坡度和高程基本上决定了土地利用的方向和方式,从而影响农业和经济的发展。石碗溪小流域面积20.73km2,为丘陵低山区。按坡度和高程对土地利用的影响程度,把坡度和高程各分为3级,即:0°～15°、15°~25°、>25°和500m以下、500~800 m、800m以上。从1:10 000地形圈上提取土地坡度和高程分级图,与土地利用现状图又叠加,获取各坡度、高程级及其土地利用类型和数据。结果表明,土地面积随坡度、海拔级的增加而加大。耕地分布在各个高程级0～15°的缓坡上,800m以上地区面积最大,果园和森林大多分布在800m以上>25°的陡坡地上。通过分析比较小流域各个行政村2002年农业总收入及种植业、林业、牧业收入与坡度和高程的关系,可以看出坡度和高程对经济发展的影响。最后,根据坡度和高程状况,结合小流域社会经济条件,提出几点建议,以其为山区小流域土地可持续利用及经济持续发展提供科学依据。  相似文献   

Mineralogy and geochemistry of granitoids from Kinnaur region,Himachal Higher Himalaya,India: Implication on the nature of felsic magmatism in the collision tectonics     

Brajesh Singh  Santosh Kumar  Masao Ban  Kazuo Nakashima 《Journal of Earth System Science》2016,125(7):1329-1352

Felsic magmatism in the southern part of Himachal Higher Himalaya is constituted by Neoproterozoic granite gneiss (GGn), Early Palaeozoic granitoids (EPG) and Tertiary tourmaline-bearing leucogranite (TLg). Magnetic susceptibility values (<3 ×10^?3 SI), molar Al₂ O ₃/(CaO + Na₂ O + K ₂O) (≥1.1), mineral assemblage (bt–ms–pl–kf–qtz ± tur ± ap), and the presence of normative corundum relate these granitoids to peraluminous S-type, ilmenite series (reduced type) granites formed in a syncollisional tectonic setting. Plagioclase from GGn (An₁₀–An₃₁) and EPG (An₁₅–An₃₃) represents oligoclase to andesine and TLg (An₂–An₁₅) represents albite to oligoclase, whereas compositional ranges of K-feldspar are more-or-less similar (Or₈₈ to Or₉₅ in GGn, Or₈₆ to Or₉₇ in EPG and Or₈₇ to Or₉₄ in TLg). Biotites in GGn (Mg/Mg + Fe^t= 0.34–0.45), EPG (Mg/Mg + Fe^t= 0.27–0.47), and TLg (Mg/Mg + Fe^t= 0.25–0.30) are ferribiotites enriched in siderophyllite, which stabilised between FMQ and HM buffers and are characterised by dominant 3Fe\(\rightleftharpoons \)2Al, 3Mg\(\rightleftharpoons \)2Al substitutions typical of peraluminous (S-type), reducing felsic melts. Muscovite in GGn (Mg/Mg + Fe^t=0.58–0.66), EPG (Mg/Mg + Fe^t=0.31?0.59), and TLg (Mg/Mg + Fe^t=0.29–0.42) represent celadonite and paragonite solid solutions, and the tourmaline from EPG and TLg belongs to the schorl-elbaite series, which are characteristics of peraluminous, Li-poor, biotite-tourmaline granites. Geochemical features reveal that the GGn and EPG precursor melts were most likely derived from melting of biotite-rich metapelite and metagraywacke sources, whereas TLg melt appears to have formed from biotite-muscovite rich metapelite and metagraywacke sources. Major and trace elements modelling suggest that the GGn, EPG and TLg parental melts have experienced low degrees (～13, ～17 and ～13%, respectively) of kf–pl–bt fractionation, respectively, subsequent to partial melting. The GGn and EPG melts are the results of a pre-Himalayan, syn-collisional Pan-African felsic magmatic event, whereas the TLg is a magmatic product of Himalayan collision tectonics.  相似文献   

山东省大汶口盆地蒸发岩地球化学特征及找钾标志          下载免费PDF全文

石厚礼  张鹏  姜赟赟 《山东国土资源》2016,32(6)

山东省大汶口盆地是我国著名的蒸发岩沉积盆地,盆地内蕴藏有丰富的石膏、岩盐等沉积型矿产。岩盐赋矿地层为古近系官庄群,控矿构造为同生正断层。通过对盆地内岩盐K,Mg等常量元素、δ~(34)S同位素特征以及盆地内盐泉卤水镁氯系数、钠氯系数进行分析,总结出盆地内蒸发岩是在相对封闭、还原的沉积环境下形成的;根据元素特征、镁氯系数及钠氯系数,总结出盆地具备成钾条件并确定找钾标志。  相似文献   

Dynamic changes of sediment load and water discharge in the Weihe River,China     

Jianxia Chang  Yunyun Li  Jie Wei  Yimin Wang  Aijun Guo 《Environmental Earth Sciences》2016,75(12):1042

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NDVI dynamic changes and their relationship with meteorological factors and soil moisture   总被引：1，自引：0，他引：1  

Hongxue Zhang  Jianxia Chang  Lianpeng Zhang  Yimin Wang  Yunyun Li  Xiaoyu Wang 《Environmental Earth Sciences》2018,77(16):582

Normalized difference vegetation index (NDVI) is an important indicator for measuring vegetation coverage, which is of great significance for evaluating vegetation dynamics and vegetation restoration. It can clearly analyze the suitable growth condition of vegetation by studying the relationship between meteorological factors, soil moisture and NDVI. Based on MODIS/NDVI data, the spatio-temporal characteristics of vegetation coverage in the Weihe River Basin (WRB) were analyzed by the trend analysis method. The relationship of NDVI with meteorological factors and NDVI with soil moisture simulated by the soil and water assessment tool (SWAT) model was analyzed in this paper. The results show that NDVI values gradually change with an increase from north to south in the WRB. The maximum of the average monthly NDVI is 0.702 (August) and the minimum is 0.288 in February from 2000 to 2015. The results of the seven grades of NDVI trend line slope indicate that the improvement area of vegetation coverage accounts for 30.93% of the total basin, and the degradation area and basically unchanged area account for 23% and 42.9%, respectively. The annual mean soil moisture is 19.37% in the WRB. There was a strong correlation between NDVI and precipitation, temperature, evaporation and soil moisture, and the correlation coefficients were 0.78, 0.89, 0.71 and 0.65, respectively. The ranges of the most suitable growth conditions for vegetation are 80–145 mm (precipitation), 13–23 °C (temperature), 94–144 mm (evaporation) and 25–33% (soil moisture), respectively.  相似文献   

A direction-dependent shear strength criterion for rock joints with two new roughness parameters     

Liren Ban  Chengzhi Qi  Chunsheng Lu 《Arabian Journal of Geosciences》2018,11(16):466

The surface morphology of a rock joint is closely related to its mechanical properties. To reasonably characterize a rock surface, two new roughness parameters were proposed in this paper. One is related to the average slope angle of asperities that contribute to the shear strength, and the other reflects the frictional behavior of asperities that is defined as the maximum possible contact area in the shear direction. Taking the standard joint roughness coefficient profiles as example, these two roughness parameters can be applied to describe the directional characteristics of shear strength. Based on their relationships with initial dilation angles, the proposed roughness parameters were incorporated into a peak shear strength criterion. It is shown that the predicted peak shear strength is consistent with experimental data, and there is a power–law relationship. The application range of new roughness parameters was determined, which may facilitate a measurement process.  相似文献   

地质-地球物理精细建模技术在庐枞下含山铁矿深部结构探测中的应用          下载免费PDF全文

王云云  兰学毅  郭冬  陶龙  马冬  丁文祥  张莎莎  叶林  李勇 《华东地质》2021,(3):293-301

为查明深部闪长岩及膏盐层与庐枞盆地内玢岩型铁矿的关系,指导盆地南西缘许家咀下含山地区的找矿工作,该文利用最新测量的重力、磁测数据,结合地表地质和钻探等先验信息,采用2.5D重磁联合反演方法建立地质-地球物理精细模型,发现二长闪长岩侵入深度为-1 200 m,岩体与中三叠统月山组接触部位发育带状膏盐层和磁铁矿化互层,类似于龙桥式矿化,表明庐枞盆地内铁矿化与闪长岩、膏盐层密切相关。该文圈定了许家咀地区下含山隆起部位两处有利找矿靶区,为下一步找矿工作指明了方向,证明了地质-地球物理综合建模方法是指导找矿的有效方法。  相似文献   

小波变换和BP神经网络模型在沉降变形监测中的应用研究     

郑云云  陈姗姗  胡勇 《测绘与空间地理信息》2019,42(2):101-103,107

变形预测在预报工程险情方面起着关键性的作用,针对施工中需及时、准确地预测变形的问题,本文利用小波变换原理对监测数据进行降噪处理,并采用BP神经网络分析不同训练样本下的预测效果和精度水平。实验结果表明:基于小波消噪后的BP网络模型,以连续的近期观测数据作为训练样本,对下期变形预测精度高,效果好,相对误差很小。因此,小波变换和BP神经网络模型在沉降变形监测工程中能作为预测研究与应用的参考。  相似文献