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V. R. Fuks 《Russian Meteorology and Hydrology》2009,34(8):528-533
An approach is proposed for analysis and interpretation of satellite measurements of oceanographic fields (sea surface temperature,
turbidity, chlorophyll concentration, and altimetry data) herein referred to as “dynamic-stochastic analysis.” This approach
consists in (1) representing spatiotemporal variability of measured characteristics as a partial differential equation which
satisfies the basic conservation lows and which is solved for the rate of change of this characteristic; (2) interpretation
of this differential equation as a multiple regression equation, where the rate of characteristic change is the predictand
and all other spatial and spatiotemporal derivatives are predictors, and (3) estimation of the regression coefficients of
this equation and their physical interpretation. This analysis was applied to satellite altimetry measurements and measurements
of primary production in the Sea of Japan and White Sea. The results are considered in this paper. 相似文献
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The Timbarra Tablelands pluton is an extensive (~550 km2) complexly zoned intrusion forming one of many predominantly monzogranite I‐type plutons, which constitute the Moonbi Supersuite in northern New South Wales, Australia. It comprises an outer rim of Rocky River monzogranite (Zones 1–3), an intermediate zone of Sandy Creek syenogranite (Zones 4A–4C), surrounding a core of Surface Hill syenogranite (Zones 5–7). The suite is calc‐alkaline, high‐K, and varies from mildly metaluminous to weakly peraluminous with increasing fractionation. Average Rb/Sr ratios range from 0.4 in the least evolved very coarse‐grained monzogranite (Zone 3) to 46 in the most evolved very fine‐grained biotite microgranite (Zone 6). Trace‐element modelling indicates that the observed compositional variation could have been produced by crystal fractionation. New bulk rock major‐ and trace‐element data for 71 samples are presented, and indicate that a compositional continuum exists that varies between 63 and 78 wt% SiO2. Importantly, there is no systematic chemical variation with spatial distribution of samples from the core of the pluton to its margin, requiring multiple separate pulses of an evolving magma to explain compositional discontinuities. The pluton is interpreted to have been emplaced at mesozonal levels (~180 ± 60 MPa, 5–10 km depth) and crystallised at temperatures between 620 and 820°C under moderately oxidising conditions (log fO2 = ‐11.5 to ‐19). The association of gold‐molybdenite mineralisation at Timbarra with moderately oxidised I‐type magmas is consistent with fractionation‐redox controls on ore‐element behaviour in magmatic systems in other studies. 相似文献
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L. Fuks I. Herdzik-Koniecko L. Maskalchuk T. Leontieva 《International Journal of Environmental Science and Technology》2018,15(10):2047-2058
Results of sorption of caesium(I), strontium(II), europium(III) and americium(III) ions on the aluminosilicates separated from the clay-salt slimes (CSS) depending on the contact time, pH, initial metal concentration are presented. CSS 1A and CSS 1B sorbents appear to be sufficiently chemically and radiation stable for practical application in treatment of the radioactive wastewaters. 相似文献
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Li-Cai Deng Heidi Jo Newberg Chao Liu Jeffrey L. Carlin Timothy C. Beers Li Chen Hsu-Tai Lee Carl J. Grillmair Puragra Guhathakurta Zhan-Wen Han Jin-Liang Hou Sebastien Lepine Jing Li Xiao-Wei Liu Kai-Ke Pan J. A. Sellwood Bo Wang Hong-Chi Wang Fan Yang Brian Yanny Hao-Tong Zhang Yue-Yang Zhang Zheng Zheng Zi Zhu 《天体物理学报》2012,(7):735-754
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Bass F. Braude S. Fuks I. Kalmykov A. Megn A. Ostrovsky I. Rosenberg A. 《Oceanic Engineering, IEEE Journal of》1977,2(1):43-52
Experiments on the scattering of radio waves in the range 200 m to 3 cm from a rough sea surface are described. Amplitude, frequency, and space-time characteristics of scattered radio signals at different states of the sea surface are presented. It is shown that the problem of the short and medium wave scattering from the sea can be solved by the perturbance method. In this case the mechanism of scattering is of "resonant" character. The intensity of the backscatter signals is proportional to the density of the spatial spectrum on the half-length of the radio waves. The high frequency radio wave scattering is well described by a two-scale model of the scattering surface, "ripple on the large wave." The intensity of scattered radio signals is also proportional to the spectrum density of "ripples" whose length is approximately equal to half a radio wave. The effect of the large waves is to modulate the amplitude of a scattered radio signal and to broaden its frequency spectrum. Methods of solution of the reverse problem were considered. This allowed determination of parameters of sea roughness by characteristics of scattered radio signals. The principles of design of the corresponding equipment are described. 相似文献
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新疆博格达造山带晚古生代构造-岩浆演化过程:火山岩组合及地球化学证据 总被引:9,自引:3,他引:6
最近,笔者在博格达山东段北部的西地-伊齐-小红柳峡一带的地质调查中发现,该区发育有大量晚石炭世柳树沟组双峰式火山岩及早二叠世卡拉岗组酸性火山岩建造,但双峰式火山岩性质及成因有别于其南侧七角井早石炭世双峰式火山岩。玄武岩富钠贫钾(K_2O=0.18%~0.45%,Na_2O=2.24%~3.63%),属拉斑系列;TiO_2=1.6%~1.7%,略高于MORB,较高的Al(Al_2O_3=16.2%~16.7%)、高Mg(MgO=8.12%~9.54%,Mg~#=61~64),以及低K_2O/TiO_2和K_2O/P_2O_5比值(分别为0.1~0.27、0.63~1.68),反映了在岩浆演化过程中分离结晶作用不明显;Rb/Sr比值0.01~0.02,Zr/Nb=21.6~39.7,Zr/Y=5.38~7.47,以及不相容元素Ba、Zr、Hf相对略富集、Nb-Ta和Th相对亏损,显示岩石具有板内玄武岩的特点;稀土元素球粒陨石标准化配分图上整体接近于平坦型,(La/Yb)_N=1.8~1.9,Eu无异常至轻微正异常(δEu=1.07~1.12),正ε_(Nd)(t)值(+5.63~+5.89),(~(143)Nd/~(144)Nd)_I=0.512927~0.512944,Th/Yb0.2,Ta/Yb=0.1,表明玄武岩浆源于亏损软流圈地幔,且在演化过程中不曾发生过斜长石的分离结晶作用,并暗示当时的大陆地壳可能由于拉张而变得较薄,玄武岩浆形成后快速上升至地表喷发。双峰式火山岩中的流纹岩Rb-Sr等时线年龄为296±2Ma(1σ),具高Si(SiO_2=76%~80%),富钾贫钠(K_2O=5.1%~5.7%,Na_2O=0.94%~2.03%);低Al(Al_2O_3=7.9%~10.4%);低Ti、Ca和P含量,属高钾钙碱性系列;微量元素Rb、Th、Zr、Hf、K相对富集,Ba、Sr、P、Ti、Nb、Ta为显著亏损;轻稀土元素适度富集且轻、重稀土分馏程度低,(La/Yb)_N=5.1~7.1,(La/Sm)_N=2、(Gd/Yb)_N=1.6~2.2,以及强烈的负Eu异常(δEu=0.17~0.2),(~(87)Sr/~(86)Sr)_I=0.7051~0.7052,δ~(18)O=11.6‰,指示岩石源于地壳物质的部分熔融,源区存在有斜长石残留,形成于大陆裂谷环境。早二叠世末流纹岩(Rb-sr等时线年龄为278±2Ma)具高Si(SiO_2=74%),富钾贫钠(K_2O/Na_2O2),低Al(Al_2O_3=11.0%)以及较低的Ti和P含量的特征,岩石为高钾钙碱性系列;微量元素PM标准化图解上表现为Rb、Ba、Th、U、K、La、Ce不相容元素相对富集,高场强元素Nb、Ta、P、Ti以及Sr为明显的负异常;轻稀土轻度富集,(La/Yb)_N=5~6,(La/Sm)_N=3,(Gd/Yb)_N=1.3~1.4,以及强烈的负Eu异常(δEu=0.31~0.39),(~(87)Sr/~(86)Sr)_I为0.7069,δ~(18)O=11.97‰,指示源于地壳物质部分熔融的产物,形成于伸展垮塌的构造环境。综合研究结果表明,博格达山前身裂谷岩浆作用始于早石炭世,结束于晚石炭世末期,早二叠世末进入后造山伸展的演化阶段。 相似文献
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目的 探讨电子束CT三维重建技术在颅颌面外科的适应症和应用价值。方法 采用美国Imatron公司的电子束CT(electron beam CT,以下简称EBCT)C-150,对76例严重颅颌面病人实行薄层CT容积扫描。将所获CT图象经数字接口传至加拿大ISG公司生产的Allegro工作站进行三维重建。结果EBCT成像技术能立体的、详尽和精确的显示机体组织三维解剖结构极其相互关系。其再现畸形或病体模型的程度可以达到近乎解剖学的精度,为准确了解和掌握病情并制定合理的手术治疗计划提供了极为重要的依据,提高了手术治疗效果。结论EBCT三维重建技术是现代颅颌面外科最主要的诊断方法之一并具有重要的临床应用价值。 相似文献
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Fuks LP 《Soviet geography》1987,28(10):756-776
"[This] paper devoted to the settlement system and the problem of rural population loss in that portion of West Siberia having a significant agricultural base takes issue with some implicit assumptions incorporated within the General Scheme of Settlement within the USSR. More specifically, policies calling for the deliberate, i.e., forced, resettlement of rural population in selected villages in order to provide economies of scale in rural services provision are criticized on two major counts: (1) that such 'enlarged' settlements will still be too small to be allocated the necessary range of functions according to standard city-planning formulae, and (2) that they accelerate rural depopulation by serving as spring-boards for migration to still larger centers." 相似文献
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