基于数字高程模型(DEM)数据的廖内省坎帕县流域地貌地质研究

Husnul Kausarian, Sandy Masdriyanto, None Batara, Adi Suryadi, Muhammad Zainuddin Lubis
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引用次数: 0

摘要

本研究在廖内省Kampar Regency地区进行,其坐标包括南纬01°00' 40" - 00°27' 00"和东经100°28' 30"- 101°14' 30"。本研究的目的是确定流域的地质条件,确定流域的地貌条件,确定流域的分区数,确定流域与降雨的关系,确定研究区与流域的地质地貌关系。采用的方法从野外取样、岩心描述、地质资料分布分析、地貌分析、流域分析、降雨分析等方面入手。通过对研究区地质资料分布的分析,从地质填图结果来看,研究区有12个地质构造,分别为:Sihapas组,Telisa组,bekasap组,Bahorok组,Farmer组,Manggala组,Talang Akar组,Telisa Atas组,Palembang Tengah组,地下室,下Palembang组成员(Air Berakat),上Palembang组成员(Muara Enim)。研究区地下地质有8个井点,进行了2次对比,分别是CR-04、CR-03、CR-01、CR-02、CR-08的第一次对比和CR-05、CR-06、CR- 07的第二次对比。地貌条件分为低地区、低丘区、丘陵区和高丘区4种。将研究区流域划分为2个流域,即Kampar流域和Siak流域。研究区2015 - 2019年5年的流域降水观测分布在5个不同的站点,降水强度波动较大
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Geomorphology and Geology Studies Using Digital Elevation Model (DEM) Data In the Watershed Area of Kampar Regency, Riau Province
This research was conducted in the area of ​​Kampar Regency, Riau Province .it was located at coordinates including 01° 00' 40" - 00° 27' 00" South Latitude and 100° 28' 30"- 101° 14' 30" East Longitude. The purpose of this study was to determine the geological condition of the watershed, and it was determined the geomorphological condition of the watershed, to determine the number of divisions of the watershed, to determine the relationship between the watershed and rainfall, to determine the geological and geomorphological relationship with the watershed in the study area. The method used starts from field sampling, core description, distribution analysis of geological data, geomorphology, watershed analysis, and analysis of rainfall. Based on the analysis of the distribution of geological data in the research area, there were 12 geological formations from the results of geological mapping, namely: the Sihapas Formation, the Telisa Formation, the bekasap formation, the Bahorok Formation, the Farmer Formation, the Manggala formation, the Talang Akar formation, the Telisa Atas formation, the Palembang Tengah formation, Basement, members of the Lower Palembang formation (Air Berakat), members of the Upper Palembang formation (Muara Enim). In subsurface geology there were 8 well points in the study area, 2 correlations were carried out, namely the 1st correlation between CR-04, CR-03, CR-01, CR-02, CR-08, and the 2nd correlation between CR-05, CR-06, CR- 07. Geomorphological conditions were divided into 4 namely lowland areas, low hill areas, hilly areas, and high hill areas. The watersheds in the research area were divided into 2 watersheds, namely the Kampar and Siak watersheds. Watershed rainfall observations in the study area for 5 years from 2015 – 2019 were located at 5 different stations, with fluctuating rainfall intensity
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