• (The) Research of the performance art and culture
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• no.40
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• pp.307-341
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• 2020

In the past, each villages of ULSAN had their own SUNGHWANGDANGs. Village folks held an annual ritual for a ghost called GOLMAEGI. That ritual, which was a form of festival supervised by the village community, was the opening of seasonal customs. People called the ritual JISINBOPKI. It was a type of NONGAK in which musicals and dramatic factors made a harmony. Usually its lyrics were called 'SUNGJUPURI'or 'JISINBOPKI' song. At that moment, villagers, thumping on the ground with their feet, danced 'DUTBEKI' to awake the sleeping ghost SUNGJUJISIN. After this ritual, the music band started to visit people's house after house around the town playing PUNGMUL NOLI which consisted of SOGO NORUM, JAPSACK NORUM. The whole proceeding of these performances did not have a definite name. Villagers prayed to SUNGJUJISIN for the prevention of bad luck in their home. This study have arranged the type of MAEGUCHIGI, which is a kind of wishing NONGAK, on the basis of two preceding primary documents. And the other is about JISINBOPKI of ULSAN district that was shown in ULSAN YUSA written by a local historian, KIM SUKBO, of ULSAN. The process of arrangement is as follows. At first, considering the implication of this NONGAK, the definite title of it was designated as ULSAN MAEGUCHIGI. And then, it was given its genre and type within NONGAK.

• Journal of The Korean Society of Agricultural Engineers
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• v.53 no.5
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• pp.9-16
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• 2011

Curve Numbers (CN) for the combination of land use and hydrologic soil group were regionalized at Imha Watershed using Long-term Hydrologic Impact Assessment (L-THIA) coupled with SCE-UA. The L-THIA was calibrated during 1991-2000 and validated during 2001-2007 using monthly observed direct runoff data. The Nash-Sutcliffe (NS) coefficients for calibration and validation were 0.91 and 0.93, respectively, and showed high model efficiency. Based on the criteria of model calibration, both calibration and validation represented 'very good' fit with observe data. The spatial distribution of direct surface runoff by L-THIA represented runoff from Thiessen pologen at Subi and Sukbo rain gage station much higher than other area due to the combination of poor hydrologic condition (hydrologic soil C and D group) and locality heavy rainfall. As a results of hydrologic condition and treatment for land use type based on calibrated CNs, forest is recommended to be hydrologically modelled dived into deciduous, coniferous, and mixed forest due to the hydrological difference. The CNs for forest and upland showed the poor hydrologic condition. The steep slope of forest and alpine agricultural field make high runoff rate which is the poor hydrologic condition because CN method can not consider field slope. L-THIA linded with SCE-UA could generated a regionalized CNs for land use type with minimized time and effort, and maximized model's accuracy.