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This study monitored reservoir sediment accumulation at two locations in the Saguling Dam reservoir, Indonesia, from December 2021 to July 2022—a period characterized by La Niña–induced wet-dry conditions—and traced sediment sources using fallout radionuclides excess 210Pb(210Pbex). At the site near the tributary inflow, immediate sedimentation patterns were observed, reaching a peak deposition rate(6.856 kg/m2) during concentrated rainfall events. Conversely, the internal reservoir site exhibited low sedimentation rates throughout the monitoring period; fine suspended materials passed through the stagnant water body, resulting in continuous influx and deposition. Based on the statistically significant differences in 210Pbex activities between forest topsoil and riverbank materials, sediment source fingerprinting revealed a higher contribution from riverbanks during the wet season. These results suggest that while overall low catchment connectivity limited the transport of slope topsoil to the stream, runoff concentrated along highly connected slopes triggered riverbank erosion and failure, delivering substantial amounts of bank material directly into the channel network system. Under prolonged wet season conditions, rapid sedimentation at the reservoir inlet occurs simultaneously with the continuous accumulation of fine-grained sediment within stagnant reservoir zones, accelerating the loss of storage capacity in the Saguling Dam. Therefore, to fundamentally mitigate reservoir siltation, tailored sediment management strategies must prioritize highly connected slopes and erosion-prone riverbank reaches alongside general topsoil conservation. The findings of this study provide foundational data for controlling sediment influx and establishing efficient, sustainable reservoir management strategies.
본 연구는 인도네시아 사굴링 댐 저수지 유역을 대상으로 라니냐에 따른 wet dry season이 나타났던 2021년 12월부터 2022년 7월까지 저수지 두 지점에서 퇴적물을 모니터링하고, 방사성동위원소를 추적자로 이용하여 퇴적물의 기원지를 추정하였다. 지류 유입부 인근 지점은 집중강우가 발생한 시기에 최대 퇴적률(6.856kg/m2)을 기록하며 즉각적인 퇴적 양상이 관측되었다. 반면, 저수지 내부 지점은 모니터링 전기간 동안 낮은 퇴적률이 나타났으며, 세립질 부유물질이 뜬짐 형태로 긴 정체 수역을 통과하여 샘플링 지점에 지속적으로 유입 및 퇴적되었다. 산사면 표토와 하안 물질의 210Pbex 값이 통계적으로 유의미한 차이를 보여 이를 추적자로 이용한 기원지 분석을 수행한 결과, 우기 동안 하안 물질이 상대적으로 더 높은 기여율을 나타냈다. 이러한 결과는 유역 전반의 낮은 연결성으로 인해 사면 표토의 하천 도달률은 낮은 반면, 고연결성 사면으로 집중된 유출수가 하안 침식 및 붕괴를 유발하여 다량의 하안 물질을 하천에 직접 공급했음을 시사한다. 특히 우기가 장기화되는 조건에서는 저수지 유입부의 급격한 퇴적과 저수지 내부 정체 수역 내 세립질 토사의 지속적 누적이 동시에 진행되어 사굴링 댐의 저수용량을 빠르게 감소시킬 수 있다. 따라서 사굴링 댐 저수지의 퇴사 문제를 근본적으로 해결하기 위해서는 유역 전반의 표토 침식 제어뿐만 아니라, 고연결성 사면 및 하안 침식 취약 구간을 최우선 관리 구역으로 선정하여 맞춤형 토사 관리 대책을 적용할 필요가 있다. 본 연구 결과는 저수지 내 유입 토사를 제어하고 효율적인 저수지 관리 전략을 수립하는데 기초자료로 활용될 수 있다.
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- Publisher :The Korean Association of Regional Geographers
- Publisher(Ko) :한국지역지리학회
- Journal Title :REGION AND GEOGRAPHY
- Journal Title(Ko) :지역과 지리
- Volume : 32
- No :3
- Pages :189-214
- DOI :https://doi.org/10.26863/JKARG.2026.8.32.3.189


REGION AND GEOGRAPHY