Aswathy M V, Vijith H, Satheesh R
Centralized Remote Sensing and GIS Facility, School of Environmental Sciences, Mahatma Gandhi University, Kottayam, 686 008, Kerala, India.
Environ Monit Assess. 2008 Mar;138(1-3):173-80. doi: 10.1007/s10661-007-9755-6. Epub 2007 Jun 12.
The present study was carried out to identify the factors influencing the sinuosity of the Pannagon river, using the IRS P6 LISS III data and Geographical Information System (GIS) on 1:50,000 scale. The river follows meandering course and exhibits a narrow, highly sinuous and incised channel. Several lines of evidence including satellite and topographic data, geological maps and field investigations and the generated themes on lithology, structure, geomorphology, slope, riparian vegetation and hydrology have analyzed to understand the controls on the channel morphology of the Pannagon river. The average of sinuosity index of the selected reaches in the river on 1967 was 1.6 and of 2004 was 1.8. The sinuous patches are more in the lower reaches of the river and most of the area comes under floodplain with thick column of alluvial deposits. The analysis shown that the style and degree of sinuosity of the Pannagon river depends on a number of geological factors, including tectonics and the riparian vegetation also plays a major role.
本研究利用印度遥感卫星P6 LISS III数据和1:50000比例尺的地理信息系统(GIS),来确定影响潘纳贡河河曲度的因素。该河流呈蜿蜒河道,展现出狭窄、高度蜿蜒且深切的河道。包括卫星和地形数据、地质图以及实地调查等多条证据线索,还有生成的关于岩性、构造、地貌、坡度、河岸植被和水文的专题数据,都已进行分析,以了解潘纳贡河河道形态的控制因素。该河选定河段在1967年的河曲度指数平均值为1.6,2004年为1.8。河曲斑块在河流下游更为密集,且大部分区域属于洪泛平原,并伴有厚厚的冲积层。分析表明,潘纳贡河的河曲样式和程度取决于多种地质因素,包括构造,河岸植被也起着重要作用。