Statistical approach to determine the salinized ground water flow path and hydrogeochemical features around the underground LPG cavern,Korea

The ground water flow path of the coastal area in the Yellow Sea, Korea, was interpreted using both the cross‐correlation analysis of hydraulic properties and the principal component analysis (PCA) of ground water chemistry. Data was obtained from observation wells in the underground liquefied petroleum gas (LPG) cavern constructed in the coastal area of Pyeongtaek. Cross‐correlation results showed that the operating pressure became more influenced on artificial factors for the variation of the groundwater level of the study area (45–66% of correlation coefficient) even though its affecting area was limited to the region with fractures or faults, and also showed that the delay time from the variation of operating pressure to the fluctuation of ground water level were relatively long periods (28–31 days). Three hydrogeochemical events (encrusted cement dissolution, host rock dissolution, and seawater intrusion), which were dominantly influenced on ground water quality, could be induced from the result of PCA. Quantitative evaluation for these events using the mixed equation with principal component scores suggest that the dissolution of encrusted cement materials was the predominant factor (39·0% of the total mixed proportion) to change the chemical composition of the seepage water during the ground water flow from the observation wells to the cavern. Integration of the statistical results also imply that ground water flow and hydrogeochemistry were predominantly affected by artificial factors such as cavern operation pressure and dissolution of encrusted cement materials, which were interdependent factors on the observation wells with high cross‐correlation coefficients and pH. Copyright © 2007 John Wiley & Sons, Ltd.     

AN OVERVIEW ON THE URBAN-RURAL INTERACTION IN THE PAST 50 YEARS IN CHINA

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On the ring current energy injection rate

Assuming that the formation of the ring current belt is a direct consequence of an enhanced crosstail electric field and hence of an enhanced convection, we calculate the total ring current kinetic energy (K_R) and the ring current energy injection rate (U_R) as a function of the cross-tail electric field (E_CT); the cross-tail electric field is assumed to have a step function-like increase. The loss of ring current particles due to recombination and charge-exchange is assumed to be distributed over the whole ring current region. It is found that: (1) the steady-state ring current energy K_R is approximately linearly proportional to E_CT; (2) the characteristic time t_c for K_R to reach the saturation level is 3–4 h; (3) the injection rate U_R is proportional to E_CT^β where β ? 1.33?1.52; and (4) the characteristic time t_p for U_R to reach the peak value is 1–2 h and the peak U_R value is 50% higher than the steady-state value. Since β is now determined specifically for an enhanced convection, an observational determination of the relationship between E_CT(or φ_CT) and U_R is essential to a better understanding of ring current formation processes. If the observed β is greater than 1.5, additional processes (e.g. an injection of heavy ions from the ionosphere to the plasma sheet and subsequently to the ring current region) may be required.     

论十九世纪德国地理学的统一性观点

“地理学要免被瓜分,就要坚持它的中心原则,这个原则就是各种自然现象和形态同人类的相关。”欧洲古希腊、罗马时代的光辉地理思想经历中世纪黑暗时代的长期窒息,其生命力日见衰竭。十六世纪的地理大发现与文艺复兴使人们的眼光既回顾到古希腊时代的地理观念,又萌生出对于地理学探讨的浓厚兴趣。但十九世纪之前的地理研究大多是抽象的哲理性的探讨和单纯的地理资料的堆砌。十九世纪以德国地理学为代表的欧洲地理学,由于洪堡和李特尔等人的富有创造性的工作,赋予了地理学以新的生机和新的个性,井促使其迅猛发展。本文旨在通过对当时哲学和自然科学发展情况的分析,论述这一时期德国地理学统一性观点的确立。     

A modeling study on steady-state and transverse dynamic motion of a towed array system

A numerical technique for mathematically modeling the steady-state and transverse dynamic motion of an underwater towed sonar array is presented. The transverse vibration response of the array is modeled using the finite difference method; the array itself is assumed to be nonneutrally buoyant and possesses a complex modulus and hence inherent damping. The results obtained from this model should provide useful information for further studying the beamforming and passive-ranging performance degradation and predicting the self-noise level of the towed array system.     

Pc1 wave generation by sudden impulses

We have studied induction magnetometer data recorded at College, Alaska for the occurrence of ULF emissions associated with sudden impulses (SI). In this study we surveyed three years of data (1977–1979 inclusively) and found that for the 76 SI's reported in IAGA bulletins, 32 were found to be followed by ULF emissions in the College data. While the 76 SI's occurred at all local times those which were associated with ULF emissions at College peaked in occurrence near local noon. We have attempted to interpret these observations in terms of a simple model based upon a Chapman-Ferraro double-dipole model of the magnetosphere. Using this model an estimate of field compressions associated with SI's can be made and from this the increases in the temperature anisotropy and plasma beta may be estimated. This simple model predicts maximum growth rate near noon on high latitude field lines, just inside the magnetopause. Further, inspection of growth rate curves for varying plasma anisotropy and beta leads us to the conclusion that an increase in anisotropy is the primary cause of the ULF emissions observed.     

A programmable microcomputer-based sonar echo processor for real-time processing

A programmable microcomputer-based sonar echo processor has been developed and field tested to process echo data in real time. The device was designed for use in fisheries acoustics and to analyze echoes from the sea floor. The instrument simultaneously performs the functions "echo integration" and "echo peak detection' on the sonar signal. The "echo integration" circuitry measures the relative acoustic energy of the echo while the "echo peak detection' electronics measure the probability density function (PDF) of the peak of the echo envelope. Each process is gated so the echoes may be processed in many short time intervals. In fisheries applications, estimates can be made of fish density (fish per unit volume), average backscattering cross section, and a combination of fish size and behavior. When using the device to analyze bottom echoes, it is possible to measure both the returned energy from the bottom sediment interfaces and the microrelief characteristics. The durability, flexibility, computer link, and floppy-disk data-storage features of the system are discussed. Data are presented of the processed echoes from biological organisms and the ocean bottom from a recent research cruise on the Atlantic Ocean near Cape Hatteras, NC. The biological results illustrated the organisms to be clearly divided into two separate spatial distributions-an observation not obvious from a standard echogram which was simultaneously used. The results from the bottom showed both 1) the difference in sub-bottom structure between two locations and 2) changes in microrelief of the water-bottom interface between another pair of locations.