• Proceedings of the Korean Information Science Society Conference
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• 2002.04b
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• pp.250-252
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• 2002

In most Multi-Agent Systems (MAS), agents are required to achieve their own goals. An agent's goals, however, can conflict with others either when agents compete with earth other to achieve a common goal or when they have to use a set of limited resources to accomplish agents'divergent goals. In this paper, we consider that a BDI architecture, as a shorthand fur belief, desire, and intention in any agent-based systems, is a core component of agents' mental attitudes and represent resource-bounded BDI agents in logic programming framework. We propose an algorithm in which BDI agents with different goals solve their problems through negotiation resolving goal conflicts.

• Proceedings of the Korean Geotechical Society Conference
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• 2002.10a
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• pp.3.2-27
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• 2002

This paper presents the status of dam construction in Korea, along with a brief assessment of the dam design and construction practice. The assessment is based on publically available design and construction records of the major existing rockfill dams which have been constructed since early 1970's, and focussed in identifying geotechnical characteristics of design and construction parameters of the dams. Though the assessment, two representative dams, having unique geotechnical characteristics, are selected for comprehensive comparison of their geotechnical engineering behavior during construction and operation. The comparison yields very interesting findings on the effects of various design and construction parameters on dam behavior.

• Journal of the Korean earth science society
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• v.25 no.6
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• pp.443-473
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• 2004

In northern Gohung granitic gneiss, porphyroblastic gneiss and migmatitic gneiss are widely distributed. Gneisses were plotted in granodiorite domain on an lUGS silica-alkali diagram. The amounts of trace elements (Li, Zn, Sc, Sr, Ni, V Y etc.) vs. $SiO_2$, somewhat decreased. Plagioclase showed a wide compositional range ($An_{32-48}$). $X_{alm}$ and $X_{sps}$ were higher in garnet rim and $X_{pyp}$ in garnet core. The rocks in the study area were formed from S and I-type magmas which generated from syn-collision and the late to post-orogenic tectonic environment. Metamorphic P-T conditions u·ere low to medium pressure, high temperature (803-913$^{\circ}C$, 6.1-7.3 kb) and overprinted by retrograde metamorphism (570-726$^{\circ}C$, 2.2-5.1 kb) and chloritization.

• Proceedings of the Korea Contents Association Conference
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• 2009.05a
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• pp.1020-1025
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• 2009

The five elements theory that people in the world objective theory is earned by a long-term observation. The key to the world and everything in the neck. The core content of this theroy is summed up in the world all things wood, fire, earth, gold, water-five material form. In the theory, the chracter's appearance, feature the five elements face is content. And the chracter's appearance, personality chracterisics and features of chracters and abstract nature of the mutual response plan which was formed way. Based on the number of world-famous cartoon chracter design analysis, special features and art theroy point the five elements the nature of man, who looks and chracter design by comparing the response of theroy and research and has the five elements. The analysis of theory and research the five elements art and people who find the nature of the systematic correlation to the future of animation, chracter design is applied.

• The Journal of Engineering Geology
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• v.15 no.1
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• pp.41-55
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• 2005

This research is aimed at investigating the ground characterization of the Cheongju granite area using the geophysical methods. Test site was chosen from the building site in Chungbuk University, Chongju, Chungbuk province. Furthermore, geophysical methods are employed on the outcrops in the east to map the distribution of fault and intrusion and reveal the degree of weathering. The subsurface structure mapped from seismic re-fraction survey mainly consists of two units of weathered soil and rock. Threshold of the units were determined on the basis of seismic velocity of 800 m/s, supported from the standard classification table. From the results of standard penetrating test(SPT), these units are found to show medium-high and high density, respectively. Weathering soil is subdivided in unsaturated layer and saturated layer with thresholds of seismic velocity (500 m/s) and resistivity (200 ohm-m). In particular, unsaturated layer is again classified into dry and wet portions using the GPR section. The boundary between unsaturated and saturated weathering soils corresponds to the groundwater table at depth of approximately 5～6.2 m, which is well correlated with the one from drill-core data. However, bedrock is not delineated by geophysical methods. In the GPR section, fault and intrusion observed on the outcrop are revealed not to extend to the building site. With respect to weathering degree, the outcrop characterized by low resistivity and velocity corresponds to the grade of 'completely weathered' from the geotechnical investigations.

• The Journal of Engineering Geology
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• v.31 no.4
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• pp.507-522
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• 2021

Specific survey objectives often cannot be met using only one geophysical method, as each method's results are influenced by the specific physical properties of subsurface materials. In particular, areas susceptible to geological hazards require investigation using more than one method in order to reduce risks to life and property. Instead of analyzing the results from each method separately, this work develops a four-quadrant criterion for classifying areas of levees as safe or weak. The assessment is based on statistically determined thresholds of seismic velocity (P-wave velocity from seismic refraction and S-wave velocity from multichannel analysis of surface waves) and electrical resistivity. Thresholds are determined by subtracting the standard deviation from the mean during performance testing of this correlation technique applied to model data of four horizontal and inclined fracture zones. Compared with results from the crossplot of resistivity and P-wave velocity, crossplot analysis using resistivity and S-wave velocity data provides more reliable information on the soil type, ground stiffness, and lithological characteristics of the levee system. A loose and sandy zone (represented by low S-wave velocity and high resistivity) falling within the second quadrant is interpreted to be a weak zone. This interpretation is well supported by the N values from standard penetrating test for the central core.

• Journal of the Korean earth science society
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• v.32 no.6
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• pp.537-547
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• 2011

Electrical resistivity tomography surveys using boreholes were applied to reveal the cause of a catastrophic land subsidence accompanied by the excessive groundwater withdrawal in urban karst area and to map the connectivity of disseminated cavities over the study area. In order to understand the hydrogeological characteristics, resistivity using exsitu core samples, groundwater level for five boreholes, and hydraulic conductivity using slug test were measured. The hydraulic conductivity variation ranging from 0.8 to $9.3{\times}10^{-4}\;cm/s$ for five boreholes and a gentle slope of groundwater level indicated that there is no significant characteristics of hydraulic heterogeneity. Core samples of the lime-silicated rock were classified as three groups including cracked, weathered, and fresh and measured the resistivity values ranged from 103 to 161, 218 to 277, and 597 to 662 ohm-m, respectively. Drilling results that showed the cavity filled with clay materials and tomogram for this region indicated resistivity value lower than 50 ohm-m. From the inverted resistivity results for each section with five boreholes, cavity and fractured layer were distributed along the depth between 10 and 20 m overall area and cavities ranging from 4 to 6 m filled with clay materials.

• Economic and Environmental Geology
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• v.38 no.3 s.172
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• pp.335-346
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• 2005

In this study, core sediments and pore water were analysed to identify the origin of organic matter and Bas in late Quaternary sediments from the northwestern Ulleung Basin of the East Sea. C/N and C/S ratios in the sediments show that the organic matter in the study area originated predominantly from marine algae. However, the results of Rock-Eval pyrolysis indicate that the organic matter has an origin of the land-plant (Type III), locating in the immature stage. These different results might be due to the heavy oxidizing of the organic matter during sinking down to the seafloor or after deposition in the sediments. Concentration of sulfate in the pore water decreases gradually with core depth, while concentration of $CH_4$ increases gradually with core depth. This indicates that sulfate reduction and methanogenesis occurred actively in the sediments. Also, it is likely that the compositions of $CH_4$ are characterized as a more biogenic origin, mostly caused by microbial activity, rather than a thermogenic one.

• Journal of the Korean earth science society
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• v.42 no.6
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• pp.677-687
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• 2021

In this study, we analyzed diatoms from core RS15-GC41 collected in Iselin Bank, Ross Sea. A total of 24 genera and 35 species of diatoms are identified, and the having valve abundance of diatoms varies from 0.2 to 28.6×10⁶/g. Four diatom assemblage zones are established by the vertical distribution of diatoms, and changed with a cycle of 100 kyrs. RS15-GC41 were deposited over the last 400 kyrs (corresponding to Marine Isotope Stages 1-11). The open-water species Fragilariopsis kerguelensis, Rhizosolenia styliformis, and Thalassionema nitzschioides abundantly occurred in interglacial periods. Whereas, Actinocyclus actinochilus abundantly dominant during the glacial periods. The distribution of these diatoms indicated, it can be seen that the sea-ice extent was larger and lasted longer during MIS 7, 9, and 11 than that of MIS 1, 3, and 5. Moreover, Paralia sulcata was abundantly predominant in MIS 7, 9, and 11; this finding suggests likely indicating that P. sulcata was transported from the coastal/inner shelf area to the study site, during accumulated in the sediments, reworked with the influx of ice-rafted debris by the currents

• Journal of the Daesoon Academy of Sciences
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• v.42
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• pp.167-199
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• 2022

A majority of religious orders in Jeungsanism believe in Jeungsan as a spiritual entity or incarnation of Maitreya. However, Daesoon Jinrihoe insists that the destiny of Maitreya lasts for fifty-thousand years and the 'gold (金)' associated with the Maitreya icon (Geumsan-sa Temple) symbolizes the 'Later World.' A different Maitreya icon was produced for Daesoon Jinrihoe's Toseong Training Temple Complex. That icon of Maitreya looks similar to the one at Gwanchok-sa Temple. That is because the icon in Daesoon Jinrihoe has been formed in order to emphasize Maitreya as a symbol different from the one in Geumsan-sa Temple. If the Maitreya icon of Geumsan-sa Temple is a core that symbolizes two figures, Jeungsan and his successor, Jeongsan, who inherited his religious orthodoxy, then the Maitreya icon at Toseong Training Temple Complex is a symbol that suggests faith and religious practice from a more conventional perspective. The Maitreya icon in Geumsan-sa Temple deals with issues of religious orthodoxy whereas the icon at Toseong is related to the prophecies on the redemption of people and the advent of Dao-empowered sages. According to Daesoon Thought, Maitreya is not just the future Buddha. He has already descended on the earth in modern times. Due to Jeungsan's descending on the earth, the incarnation of Maitreya has been accomplished as far as the Daesoon faith is concerned. Henceforth, the true practice of Maitreya reverence in the context of Daesoon Jinrihoe should be focused around a group of devotees who specifically practice Jeungsan's Reordering Works of Heaven and Earth. An attempt to do so will enable the formation of the ideal world aimed upon by Maitreya.