Raharjo, Sugeng and Teguh Paripurno, Eko and Hartadi, Joko and Oktavia Alfani, Dewi (2017) The Movement of Lineslide Based on Geodetic Data in Clapar Area, Banjarnegara Regency, Central Java. Journal of Techno, 3 (1). pp. 74-86. ISSN 2461-1484
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Jurnal Techno, Vol.03, No.1, Agustus,2017.pdf Download (6MB) | Preview |
Abstract
Landslide disaster is one of the most occur disasters in Clapar, Banjarnegara. Landslide is a recurring event and until now there is no suitable method to respond to the threat, so the preventive stage have not been maximized. According to the research that the movement of land in the area is very active but can not be known qualitatively or quantitatively the level of activity n cause landslides. This research is expected to help related parties to design la mitigation in Clapar Banjarnegara district so as to reduce the loss of both infrastructure or soul in the future. While the long-term goal ofthis rescarch is to make map clearly the landslide prone areas so that it can facilitate in modeling to design of disaster mitigation. ethod used in the achievement ofthe objective is calculating the movement ofthe la und positioning observed over a period of time, analyzing the movement using nce difference test, congruency test and point movement test, compile the m fmitigation design of landslide disaster in the research area. In addirion t0 ntific meetings and journals, research resulis will also be informed to relevant lic through the medium of information with simple language so that more eas by the public and can be applied directly. Based on the statistical test of land movement indicates that the test results are accepted, then congruency test and point movement test to better ensure results that have been obtained from parameters significance difference test. Based on the results of the congruency test and point movement test obtained the same results with parameters significance difference test, the test results are accepted. It shows that the horizontal and vertical movement values occurring at the period of I up to III, II up to III and the I up to III are not caused by the movement of the land, but due to random errors in the measurements in the first, second, and third period. The results of statistical tests show that which appropriate with the condition when the measurement was in conditions before the rain, while the landslide occurs in after rain Keywords : landslide, lithologi, hazard, clapar, banjarnegara
| Item Type: | Article |
|---|---|
| Uncontrolled Keywords: | landslide, lithologi, hazard, clapar, banjarnegara |
| Subjects: | Q Science > QE Geology |
| Depositing User: | Dr..Ir. MT Sugeng Raharjo |
| Date Deposited: | 24 Feb 2022 07:38 |
| Last Modified: | 24 Feb 2022 07:39 |
| URI: | http://eprints.upnyk.ac.id/id/eprint/27557 |
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