ScholarWorks@Gyeongsang National University: Park, Jae Hyeon

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Park, Jae Hyeon (박재현)

농업생명과학대학 (환경산림과학부)

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Tel 0557513248
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landslide:7||땅밀림:6||land creep:5||Quarry:5||soil bulk density:4||crack:4||forest management:3||Forest road cutslope:3||Land creeping:3||stemflow:3||landcreep:3||quarry:3||restoration:3||a karst physiognomy:3||Guizhou:3||Gabion system:3||Soil bulk density:3||slowmoving landslide:3||prevention of the stone hazarding:2||the Sangrim Woodlands Natural Monument:2||the Songrim woodland restoration:2||the access restriction area:2||Afforestation:2||Biomass by land types:2||Landcreep:2||Soil restoration:2||electrical conductivity:2||Mean salt concentration:2||rehabilitation:2||Soil creeping:2||colluvial soil:2||the slow – moving landslide:2||afforestation:2||the torrent control structure:2||Sediment:2||Bulk density:2||soil and stream water quality.:2||throughfall:2||soil moisture content:2||Ecological restoration:2||The capacity of soil water conservation:2||Soil hardness:2||triggering factor:2||Slope stability.:2||silvicultural practices:2||Soil erosion mass:2||vegetation base materials:2||Slowmoving landslide:2||forest trail:2||토양경도:2||debris flow:2||soil strength:2||Erode control soil:2||Songrim Woodland Natural Monument:2||vertical quarry wall:2||ground water movement:2||stream bank:2||stream water quality:2||Revegetation:2||disolved oxygen:2||Management status:1||Mattress system:1||Mesopore ratio.:1||Microtopography:1||Mixing ratio of seeds.:1||Monitoring:1||Mountain stream:1||Mt. Geumgang:1||NTRIP service:1||Namgang Dam reservoir area:1||Occurrence Area:1||Occurrence Distribution Rate:1||Officer:1||Organic constituent:1||Overturn:1||Plant cover:1||Prevention of mountain disasters:1||Rainfall intensity:1||Rehabilitation:1||Reservoir:1||Restoration effort:1||Restoration of quarries:1||Rock desertification:1||SWOT analysis:1||Sedimentary bedrocks:1||Sedimentary rocks:1||Shoot growth increment:1||Sliding:1||Slope failure and erosion:1||Soil and stream water quality:1||Soil characteristics:1||Soil condition:1||Soil physical properties:1||Soil strength:1||Stability.:1||Stemflow:1||Stone gradestabilization:1||Stream conservation:1||Stream water:1||Strip road:1||Succession.:1||Tension crack:1||The desert afforestation:1||The discontinuity slopes:1||The rate of existence of forestation plant:1||Throughfall:1||Torrent erosion control work:1||Travel Writing:1||Vegetation Restoration.:1||Vegetation base materials:1||Vertical quarry wall:1||Visiting roads of stream of Chilsun in Jirisan:1||Water permeability:1||Water quality:1||Water retention capacity:1||Weathered rock:1||Widening direction:1||Wood meal:1||a harmony of beauty landscape:1||angle of curved trees:1||aspect ratio:1||bedrock landslide:1||berm:1||black shale:1||broadleaved evergreen:1||bulk density:1||carbon:1||catchment area:1||cation exchange capacity:1||chinese minnow:1||clay soil landslide:1||colluvium landslide:1||communication space:1||coverage:1||cracks:1||cutting slopes:1||dam use of tetrapod:1||depression:1||deregulation:1||discontinuous surface:1||dissolved oxygen:1||electrical resistivity method:1||electrical resistivity test:1||electrolyte leakage test:1||evenness:1||expressway:1||fertilization:1||forest:1||forest disease:1||forest environmental characteristics:1||forest fertilization:1||forest fire:1||forest road constructions:1||forest trails:1||forest watershed:1||forestry:1||gabion:1||gabion systems with vegetation base materials:1||gabion wall system:1||geological and soil properties:1||geophysical exploration:1||green dam:1||green restoration planning:1||greening type:1||groundwater:1||groundwater flow:1||growth characteristics:1||land creeping:1||land slide. .:1||landscape view preference:1||landslide hazard class:1||landslide hazard map:1||law:1||lethal temperature:1||linear interpolation:1||litter fall:1||livelihood environment forest protected areas:1||longitudinal section form ratio:1||lower than the average slope of mountain:1||management:1||maximum daily rainfall events:1||mean electric conductivity:1||mesopore ratio:1||microtopography:1||microtopography:1||mining:1||movement of fishes and snials:1||naturally good ecological potential of forest road cutslope:1||nitrogen:1||nonlinear regression:1||nutrient cycling:1||oak:1||open type structures:1||organic composts:1||orographic precipitation:1||overturning:1||parent rock:1||peat moss:1||phosphorus:1||physicochemistry:1||pine wilt disease:1||pit slope:1||potassium:1||pruning:1||quarrying industry:1||rainfall:1||regrowth test:1||regulation:1||restoration effort:1||restoration measures:1||restoration type:1||retaining wall:1||revegetation:1||runoff ratio:1||sawdust:1||scar:1||scenic view preference:1||seismic survey:1||sinkhole:1||sliding:1||slope failure and erosion:1||slope stability:1||slope type:1||slow–moving landslide (landcreep):1||slowmoving landslide hazard classes:1||soil compaction:1||soil erosion:1||soil erosion control:1||soil hardness:1||soil physical properties:1||soil physical property:1||soil physicochemical property:1||soil property:1||soil restoration plan:1||solifluction soil인하여 용존되는 이온이 증가하기 때문이라고 하였다.Murdoch et al. (2000)은 봄에 온도 상승으로 인한 융설수가 동결융해침식 토사와 함께 수질저하를 발생시키는원인이며:1||species diversity index:1||stone debris:1||structure stability:1||tension crack:1||the RestYear System areas:1||the construction guidelines of soil erosion control structures for a restoration:1||the cutting and banking slopes:1||the discontinuity slopes:1||the facility application type:1||the leisure facility type:1||the opportunity factors:1||the rates of pore space:1||the sedimental deposit soil:1||the slow–moving landslide:1||the strength factors:1||the tree planting type:1||the water quality:1||thinning:1||throughfall를 분석하였다. 이때 pH(pH meter:1||topography:1||trail damage types:1||treerings:1||urban forest:1||urban soil:1||vegetation:1||vegetation cover percentage:1||vegetation restoration:1||vegetationbased gabion:1||vulnerability criteria:1||waterway:1||weathered rock landslide:1||감숙성 백은시 사막지역:1||계류보전:1||공무원:1||관리현황:1||금강산:1||녹화 효과:1||대형무척추동물:1||돌바닥막이:1||등 (1999)은 융설수의 화학적조성이 유럽과 북미지역에서 산림생태계에 심각한 영향을 미치고:1||땅밀림 산사태:1||미세지형:1||발생면적:1||발생분포율:1||방류수:1||백악기:1||복구:1||불연속면:1||붕적토:1||사막화:1||사방댐:1||사방지:1||산림문화:1||산림환경특성:1||산사태:1||산사태 복원:1||산사태위험등급:1||산재재해 방지:1||산지계류:1||생태적 복원:1||석학:1||수간유하수를 채취한 전나무와 잣:1||수질:1||숙박시설:1||식생기반재:1||식생기반재돌망태기슭막이:1||신초생장량:1||야계사방사업:1||여행필기:1||의식 분석:1||이로 인해 생태계까지 좋지 않은 영향을 미친다고 하였다. 또한:1||인장균열:1||저비저항이상대:1||저서성:1||전기전도도(EC meter:1||절리간격:1||종단형상비:1||지질적 요인:1||지하수 유동:1||침사지:1||쿠부치사막:1||토석류:1||토석사업장:1||토석채취지:1||토양용적비중:1||토양특성:1||퇴적암:1||평면형상비:1||풍화암:1||피복율:1||하천수:1||항공사진:1||활동연약대:1||Accommodation Facilities:1||활착율:1||Accumulative rainfall:1||Active weak zone:1||Aerial photographs:1||Amount of soil erosion:1||Artificial structures:1||Aspect ratio:1||Benthic Macroinvertebrates:1||Biochar:1||Bughansan National Park:1||CM11P)는 항목의 특성상 현장에서 시료채취시 즉시 측정하였다. 자료의 분석을 위하여 산림시업에 따른 pH 및 전기전도도의 관계는 spss/pc± 를 이 용해 직선회귀분석을 실시하였다.2. 조사대상지의 임황수관통과우:1||Chaos:1||Classical Scholars:1||Climax forest:1||Colluvial debris types:1||Colluvial soil:1||Consciousness:1||Conservation of valley ecosystem.:1||Continuity:1||Coverage:1||Cretaceous period:1||DGNSS central office:1||Dam use of Tetrapod:1||Debris flow:1||Desertification in Kubuqi Desert area:1||Dispersibility of soil:1||Distribution characteristics:1||Echo sounder:1||Effluence:1||Electrical Power:1||Electrical conductivity:1||Environmentfriendly ways:1||Erosion control dam:1||Forecast:1||Forest Culture:1||Forest environmental factors:1||Forest landslide:1||Forest management:1||Forest road cut:1||Gabion Systems with Vegetation Base Materials revetment:1||Gansusheng Baiyin desert area:1||Geological factors:1||Geospatial characteristics:1||Grit chamber:1||Ground water movement:1||Growing media:1||HI8314):1||Hydrographic survey:1||Improve ecological environment in slopes of an expressway:1||Joint space:1||Kandslide frequency:1||Land creep:1||Landscape analysis:1||Landslide:1||Landslide hazard grade:1||Landslide(Creeping):1||Landslidetriggering factors:1||Longitudinal section form ratio:1||Low resistivity zone:1||Lyapunov Exponent:1||

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