SEDIMENTASI DI SUNGAI JENEBERANG DAN WADUK BILI-BILI AKIBAT LONGSOR DI DAS JENEBERANG
| Main Author: | Solle, Muchtar Salam |
|---|---|
| Format: | Article |
| Terbitan: |
JURNAL ECOSOLUM VOLUME 1 NOMOR 2, SEPTEMBER-DESEMBER 2012, JURUSAN ILMU TANAH FAKULTAS PERTANIAN UNHAS
, 2015
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| Subjects: | |
| Online Access: |
http://repository.unhas.ac.id/handle/123456789/13484 |
Daftar Isi:
- Collapsed of Caldera-wall of Mt. Bawakaraeng occurred on March 26, 2004. The caldera is situated at elevation 2,600 m above MSL and is the headwaters of Jeneberang river. The volume of collapsed mass was estimated 200 ??? 3000 million M3 and it closed Jeneberang river channel along 7 km. One month after the collapsed, mud flow occurred and covered paddy field along the Jeneberang river. Up to now the mud flow frequently occurred, especially in the rainy season. The river discharge containing a high density of sediment has been flowing down into Bili-Bili reservoir and it is anticipated that its lifetime would be shorter and the water quality of municipal water would be deteriorited.