Article Per Year (5 Year)
p-Index From 2021 - 2026
0
P-Index
This Author published in this journals
All Journal TEKNIK Jurnal technoscientia JURNAL TEKNOLOGI TECHNOSCIENTIA
Arief Mustofa Nur
Unknown Affiliation
Chemical Engineering, Chemistry & Bioengineering Computer Science & IT Earth & Planetary Sciences Engineering Industrial & Manufacturing Engineering Materials Science & Nanotechnology Mechanical Engineering

Published : 3 Documents Claim Missing Document
Claim Missing Document
Check
Articles

Found 3 Documents
Search

 1 
GERAKAN TANAH DI KARANGSAMBUNG, PENYEBAB DAN ANTISIPASI PENCEGAHANNYA Mustofa Nur, Arief
JURNAL TEKNOLOGI TECHNOSCIENTIA Academia Ista Vol 12 No 01 Agustus 2007
Publisher : Lembaga Penelitian & Pengabdian Kepada Masyarakat (LPPM), IST AKPRIND Yogyakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (736.152 KB) | DOI: 10.34151/technoscientia.v0i0.1975

Abstract

Land movement or better known as landslide represents one of the geologic ha-zard often occur in Indonesia including Karangsambung. Landslide basically occurs as a result of slope instability. The aim of this researh was to study factors affecting land mo-vement. The objective of this study was to determine anticipatory steps that can be per-formed by the community itself. The method used was by observation and morphological analysis of the land movement, geological aspect, hidrological aspect, and aspect of landuse. Based on the observed data and literature study, there are two types of landslide movement in Karangsambung area, i.e. creep type at small slope (3°-5°) and slump type at high slope (60°). The mechanism causing land movement in the research location is estimated to be clays that is thick enough to join each others at bedrock in the form of claystone Karangsambung Formation having the character of waterproof. Existence of o-ther factors such as inclination of slope and hidrology progressively trigger the land mo-vement. This condition caused trigger force bigger than supported force, so that the land easier to move. Anticipatory steps that can be done are by closing cracking land, preventing sur-face water enter into land movement area, making stone bagwark and bamboo, and also the people are advised to set aside to safer places if heavy rain comes.
KAJIAN GEOLOGI LINGKUNGAN PADA LOKASI PENAMBANGAN BATUAN DIABAS GUNUNG PARANG DALAM RANGKA KONSERVASI BATUAN DI CAGAR ALAM GEOLOGI KARANGSAMBUNG Mustofa Nur, Arief
TEKNIK Volume 32, Nomor 2, Tahun 2011
Publisher : Diponegoro University

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (567.363 KB) | DOI: 10.14710/teknik.v32i2.1697

Abstract

Diabas Parang hill is one of location which conservated in area conservation of geological Karangsambung.Now, it is threatened, because there are many mines at surrounding it. Activities of mining not care science andenvironmental conservation.Impact of mining so cause change of topography/morphology, slope become more steep, and mining locationbecome potentially accure rock fall and landslide. Pursuant to result of laboratory analysis, engineeringproperties diabas Parang hill strongless than andesit so it is only fulfil for trotoir.For diabas conservation which is protected so need affort to stop activity of mining. The effort can do seekingaltenative location for mine and/or to change mine activities.
GERAKAN TANAH DI KARANGSAMBUNG, PENYEBAB DAN ANTISIPASI PENCEGAHANNYA Mustofa Nur, Arief
JURNAL TEKNOLOGI TECHNOSCIENTIA Academia Ista Vol 12 No 01 Agustus 2007
Publisher : Lembaga Penelitian & Pengabdian Kepada Masyarakat (LPPM), IST AKPRIND Yogyakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.34151/technoscientia.v0i0.1975

Abstract

Land movement or better known as landslide represents one of the geologic ha-zard often occur in Indonesia including Karangsambung. Landslide basically occurs as a result of slope instability. The aim of this researh was to study factors affecting land mo-vement. The objective of this study was to determine anticipatory steps that can be per-formed by the community itself. The method used was by observation and morphological analysis of the land movement, geological aspect, hidrological aspect, and aspect of landuse. Based on the observed data and literature study, there are two types of landslide movement in Karangsambung area, i.e. creep type at small slope (3°-5°) and slump type at high slope (60°). The mechanism causing land movement in the research location is estimated to be clays that is thick enough to join each others at bedrock in the form of claystone Karangsambung Formation having the character of waterproof. Existence of o-ther factors such as inclination of slope and hidrology progressively trigger the land mo-vement. This condition caused trigger force bigger than supported force, so that the land easier to move. Anticipatory steps that can be done are by closing cracking land, preventing sur-face water enter into land movement area, making stone bagwark and bamboo, and also the people are advised to set aside to safer places if heavy rain comes.
Co-Authors