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31.
红壤丘陵小区域水平上不同时段土壤质量变化的评价和分析 总被引:39,自引:1,他引:39
引相相对土壤质量指数的概念,应用地理信息系统技术,为小区域水平上土壤质量时空变化的评价提供了一种方法,并用于千烟洲试验站开垦利用11a后土壤质量变化的评价。统计分析服农田,桔园,牧草地,人工林,天然林等多种土地利用方式下土壤质量变化的特征。 相似文献
32.
龚育龄 《华东地质学院学报》1996,19(3):254-261
本文从理论上对相关分析法区分重力异常的可行性进行了论述,并从一元线性回归方程着手,对大地水准面上的重力值与相应的地形高程作了相关分析,通过分析,认为在区域性小比例主均衡补偿基本完善的条件下,重力值与高程有极好的线性相关关系;当计算窗口较大时,地下的局部不均匀体,不足以破坏重力值与高程的相头发一,所以,在实际工作中,利用相关分析处理重力资料的叠加场,可以收到较好的效果,且方法简单易行。 相似文献
33.
Song-Yan Song Xue-Song Zhou Chun-Yong Wang Xian-Kang Zhang Jian-Li Song Yi Gong 《地震学报(英文版)》1997,10(1):15-25
On the basis of S wave information from Tai’an-Xinzhou DSS profile and with reference to the results from P-wave interpretation,
the 2-D structures, including S-wave velocity V
s, ratio γ between V
p and V
s; and Poisson’ s ratio σ, are calculated; the structural configuration of the profile is presented and the relevant inferences are drawn from the
above results. Upwarping mantle districts (V
s≈4.30 km/s) and sloping mantle districts (V
s≈4.50 km/s) of the profile with velocity difference about −4% at the top of upper mantle are divided according to the differences
of V
s, γ and σ in different media and structures, also with reference to the information of their neighbouring regions; the existence of
Niujiaqiao-Dongwang high-angle ultra-crustal fault zone is reaffirmed; the properties of low and high velocity blocks (zones)
including the crust-mantle transitionalzone and the boudary indicators of North China rift valley are discussed. A comprehensive
study is conducted on the relation of the interpretation results with earthquakes. It is concluded that the mantle upwarps,
thermal material upwells through the high-angle fault, the primary hypocenter was located at the crust-mantle juncture 30.0∼33.0
km deep, and additional stress excited the M
S=6.8 and M
S=7.2 earthquakes at specific locations around 9.0 km below Niujiaqiao-Dongwang, the earthquakes took place around the high-angle
ultra-crustal fault and centered in the brittle media and rock strata with low γ and low σ values.
This subject is part of the 85-907-02 key project during the “8th Five-Year Plan” from the State Science and Technology Commission. 相似文献
34.
偏振激发能量色散X荧光法在地球化学分析中应用及其与波长色散X荧光法的比较 总被引:1,自引:0,他引:1
偏振激发能量色散X射线荧光光谱(P-EDXRF)技术是20世纪末出现的新分析技术。国内采用X-Lab2000型仪器的初步研究表明,在总计数时间为600秒时,可以对近30种元素进行定量,检出限为0.5-30μg/g,与国际上发表的文献值基本一致。本工作通过约100个实际样品分析,并与波长色散X射线荧光法(WDXRF)分析结果的比较,对P-EDXRF的分析性能进行了评价。与WDXRF相比,P-EDXRF法具有分析速度快、设备购置费用低、运行成本低、全谱同时采集(有利于发现元素含量异常)等优点,因此特别适合地球化学填图样品的快速分析。而WDXRF在精度要求较高的分析中更具竞争力。 相似文献
35.
龚新华 《地震地磁观测与研究》2005,(Z1)
长沙地震台北东方向深源地震的记录中,发生于日本海边缘和中朝俄接界区域的深源地震存在sP震相,它超前于S波,由于震相能量较大,容易与S波相混淆。本文讨论了如何对它进行辨别。 相似文献
36.
37.
Validating the ability of the discontinuous deformation analysis method to model normal P‐wave propagation across rock fractures
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The effects of fractures on wave propagation problems are increasingly abstracting the attention of scholars and engineers in rock engineering field. This study aims to fully validate the ability of discontinuous deformation analysis (DDA) to model normal P‐wave propagation across rock fractures. The effects of a single fracture and multiple parallel fractures are all tested. The results indicate that DDA can accurately reflect the fracture effects, including the fractures stiffness, the fracture spacing and the fracture number, and the effects of incident wave frequency on one‐dimensional P‐wave propagation problems. Thus, DDA is able to deal well with normal incident P‐wave propagation problems. Copyright © 2017 John Wiley & Sons, Ltd. 相似文献
38.
39.
Q. Liu Y.‐B. Wu H. Wang S. Gao Z.‐W. Qin X.‐C. Liu S.‐H. Yang H.‐J. Gong 《Journal of Metamorphic Geology》2014,32(2):177-193
Migmatites are predominant in the North Qinling (NQ) orogen, but their formation ages are poorly constrained. This paper presents a combined study of cathodoluminescence imaging, U–Pb age, trace element and Hf isotopes of zircon in migmatites from the NQ unit. In the migmatites, most zircon grains occur as new, homogeneous crystals, while some are present as overgrowth rims around inherited cores. Morphological and trace element features suggest that the zircon crystals are metamorphic and formed during partial melting. The inherited cores have oscillatory zoning and yield U–Pb ages of c. 900 Ma, representing their protolith ages. The early Neoproterozoic protoliths probably formed in an active continental margin, being a response to the assembly of the supercontinent Rodinia. The migmatite zircon yields Hf model ages of 1911 ± 20 to 990 ± 22 Ma, indicating that the protoliths were derived from reworking of Palaeoproterozoic to Neoproterozoic crustal materials. The anatexis zircon yields formation ages ranging from 455 ± 5 to 420 ± 4 Ma, with a peak at c. 435 Ma. Combined with previous results, we suggest that the migmatization of the NQ terrane occurred at c. 455–400 Ma. The migmatization was c. 50 Ma later than the c. 490 Ma ultra‐high‐P (UHP) metamorphism, indicating that they occurred in two independent tectonic events. By contrast, the migmatization was coeval with the granulite facies metamorphism and the granitic magmatism in the NQ unit, which collectively argue for their formation due to the northward subduction of the Shangdan Ocean. UHP rocks were distributed mainly along the northern margin and occasionally in the inner part of the NQ unit, indicating that they were exhumed along the northern edge and detached from the basement by the subsequent migmatization process. 相似文献
40.
Accepting the concept of standardization introduced by the standardized precipitation index, similar methodologies have been developed to construct some other standardized drought indices such as the standardized precipitation evapotranspiration index (SPEI). In this study, the authors provided deep insight into the SPEI and recognized potential deficiencies/limitations in relating to the climatic water balance it used. By coupling another well‐known Palmer drought severity index (PDSI), we proposed a new standardized Palmer drought index (SPDI) through a moisture departure probabilistic approach, which allows multi‐scalar calculation for accurate temporal and spatial comparison of the hydro‐meteorological conditions of different locations. Using datasets of monthly precipitation, temperature and soil available water capacity, the moisture deficit/surplus was calculated at multiple temporal scales, and a couple of techniques were adopted to adjust corresponding time series to a generalized extreme value distribution out of several candidates. Results of the historical records (1900–2012) for diverse climates by multiple indices showed that the SPDI was highly consistent and correlated with the SPEI and self‐calibrated PDSI at most analysed time scales. Furthermore, a simple experiment of hypothetical temperature and/or precipitation change scenarios also verified the effectiveness of this newly derived SPDI in response to climate change impacts. Being more robust and preferable in spatial consistency and comparability as well as combining the simplicity of calculation with sufficient accounting of the physical nature of water supply and demand relating to droughts, the SPDI is promising to serve as a competent reference and an alternative for drought assessment and monitoring. Copyright © 2013 John Wiley & Sons, Ltd. 相似文献