Identification and Prediction of Dip Slope by API and GIS Approach
Jin-King Liu
Research Scientist
Energy and Resources laboratories, Itri
L200, ERL/ITRI, Shin-Chu Hsien 310, Taiwan
Tel :+886-3-591-6352; Fax: +886-3-582-0017
E-mail: F660124@erl.itri.org.tw
Abstract
Rocks of Taiwan Island are highly fractured. Hazardous landslides takes place very often in rainy season, especially typhoon season. since the damage caused by Typhoon Herb of 31/July/1996 was estimated more than NT$10 billions, as project to conduct a general survey of exaction landslides of the whole island employing aerial photo-interpretation (API) and GIS techniques was launched for the first step to the preventive measures. Various types of landslides on basis of API are identified are defined, as a contrast to conventional landslide classification scheme. one of the major types of the landslide hazards is the dip slope failure where the dip-direction of rock formation is sub parallel to he look-direction of slope. With the processing of datasets of DTM and rock formations, the areas prone to dip slopes hazards can be predicted. And, subsequently, these areas are further compared with the landslides interpreted from aerial photographs to verify the prediction. this approach proves to be effective.
1.Introduction
Taiwan Island is located at tectonically active region where relocks are highly fractured. Thus hazardous landslides take place all the time when torrential rainfall comes in rainy season, especially in Typhoon season. One of the major types of hazards is the dip slope failure where the dip-direction off rock formation is sub-parallel to the look-direction of slope sloping land are fragile ad sensitive. However, the high rising price of urban lands has urged the people to approach the marginal lands with potential landslide hazards. Thus, regulations are enforced to restrict the development of areas prone to dip slope hazard.
With the processing of a dataset of DTM (i.e. Digital Terrain Model ) and a dataset of the attitude of a rock formation, it is possible to map the areas where are prone to dip slope hazard. And, for verification of these areas, results were further compares with the landslides interpreted form aerial photographs, taken in 21/june/1990, and 14/July/1997. A case form Tauyen Country of northern Taiwan is given in this paper to demonstrate the process.
2.General Survey is Critical
The damage caused by Typhoon Herb on July 30-August 1 of 1996 was estimated more than NT$10 billions besides the loss of lives. Thus, a project to conduct a general survey of existing landslides of he whole Taiwans Island employing aerial photo interpretation (API) and GIS techniques was deemed necessary for the first step to the preventive measures. the project was launched on 1 July 1997 and it will last for 4 years to finish the interpretation and a resulted database on basis of circa 20000 aerial photos. A task force lead by author is dedicated to this project.
There phases are devised for each year, namely the standard API phase, the field check phase, and the database phase. In the standard AAPI phase, aerial photos of the study area of the fiscal year area interpreted with standard API procedure as adopted by photo-geologist. Various types of landslides are transferred to orthophoto map with a scale of 1:5000 ( in low relief terrain ) and 1:1000 ( in mountainous terrain ) and each landslide is assigned a unique ID number. In the field check phase, the features of each landslide are recorded along with a picture an assort video using digital cameral and digital VCR. In the database phase, a landslide digital map is accomplished with a database, which includes the map, the features table, the picture and the video of each landslide of the study area.
In this study, various types of landslides on basis of API are identified and defined, as a contrast to conventional landslide classification scheme, which is not based on aerial view and is devised to describe a single landslide rather than a regional study of landslides (Liu et., 1998).
3.Gis for Predicting Dip Slopes
3-1 Dip Slopes
Bedding planes are discontinuities of rock bodies. The geometry of bedding planes in relation to slope planes is a critical factor to the slope stability. Relatively, oblique and reverse slopes are stable in comparable to dip comparable to dip slopes, as shown in figure 1 ( Liu, 1985 a and y 1985b). road A is on a reverse slope, whereas Road B on a dip slope.
Figure 1. Road alternatives. Road a is on a reverse slope, whereas Road B is on a dip slope.
A dip slope is a slope where the dip direction of rock bedding is sub-parallel to the look direction of a slope. On a dip slope, if the slope angle is less than the dip angle ( figure 2a ), the bedding plane runs into the ground. Therefore, a stable condition cab be presumed provided no other special conditions. On the contrary, if the dip angle is less than the slope angle on a dip slope ( figure 2 b), the bedding plane enlights on the slope. And, the bedding plane of sedimentary rocks is basically a weak plane apt to becoming a gliding surface. Therefore, the later case is relatively unstable.
Figure 2. Dip slopes are common in sedimentary rock terrain, where 2a is a stable dip slope and 2b is a stable dip slope and 2b is a unstable dip slope.
The physiographic environment of the study area is characterized by several features vulnerable to dip slope landslides. The most important are,
- It is located in a geologically active region, where the Eurasion Tectonic Plate collides with Philippine Sea Plate. Strata are intensively folded. Joints and other fractures are well developed (Liu et at, 1983)
- The geology is primarily a sandstone and shale alternation. the contrast between sandstone and shale easily accumulates water percolated from the permeable top layer or from fractures to the top surface of the shale formation.
- Heavy precipitation takes place throughout the year, especially during the typhoon season between May and August.
