Assessing landform patterns and resource potentials using digital terrain models
Loading...
Date
Journal Title
Journal ISSN
Volume Title
Publisher
Postgraduate Unit, Faculty of Arts and Culture, South Eastern University of Sri Lanka.
Abstract
This study effectively demonstrates the power of Digital Terrain Models (DTMs) in detailed micro
level mapping and landform pattern analysis, proving particularly valuable for large-scale cadastral
initiatives. Integrating GIS and remote sensing techniques, DTMs enable nuanced spatial
evaluations and richer visual representations. The research methodology incorporated a synergistic
blend of existing cadastral maps, elevation data sourced from SRTM and ALOS DEM, field
collected GPS readings, and pre-existing Digital Elevation Model (DEM) data. This integrated
approach yielded several significant outcomes for detailed micro-level mapping. Specifically,
DTMs facilitated a deeper understanding of the physiographic arrangement and the identification
of areas susceptible to erosion. Furthermore, they aided in comparing soil distribution patterns,
revealing homogeneity or heterogeneity, while 3D visualization capabilities allowed for the analysis
of intricate soil-geomorphic and physiographic interrelationships. In conclusion, the study
underscores the effectiveness of DTMs in micro-level spatial investigations, especially for mapping
small villages or watersheds to pinpoint erosion-prone zones. This was followed by an analysis of
soil-physiographic relationships and the potential for land resource mapping, ultimately assisting
in the identification of critical water conservation hotspots. Ultimately, DTMs present a cost
efficient methodology for natural resource mapping and streamlining field survey operations.
Description
Citation
Two-Day Multi–Disciplinary International Conference - Book of Abstracts on "Digital Inequality and Social Stratification" - 2025 (Hybride Mode), 20th-21th 2025. Postgraduate Unit, Faculty of Arts and Culture, South Eastern University of Sri Lanka. pp. 20.
