- Hydrology and Watershed Management Studies
- Flood Risk Assessment and Management
- Hydrology and Drought Analysis
- Soil and Unsaturated Flow
- Landslides and related hazards
- Soil erosion and sediment transport
- Water resources management and optimization
- Hydrological Forecasting Using AI
- Hydrology and Sediment Transport Processes
- Cryospheric studies and observations
- Geotechnical Engineering and Soil Stabilization
- Geotechnical Engineering and Analysis
- Dam Engineering and Safety
- Research studies in Vietnam
- Groundwater and Watershed Analysis
- Water Systems and Optimization
- Climate variability and models
- Plant Water Relations and Carbon Dynamics
Suranaree University of Technology
2009-2021
Institute of Engineering
2016-2017
The University of Western Australia
2000-2009
Observed differences between water balance for temperate and semiarid catchments can be attributed to variability in the primary controls of soil profile (soil storage capacity permeability), vegetation (surface coverage use efficiency), climate (rainfall potential evaporation). Motivated by downward development methodology mooted Klemes [1983], this paper explores underlying landscape interactions that cause a number benchmark around Australia. A systematic parsimonious analysis based...
Two uses of the terms “linearity” and “nonlinearity” appear in recent literature. The first definition nonlinearity is with respect to dynamical property such as rainfall‐runoff response a catchment, this sense refers nonlinear dependence storm on magnitude rainfall inputs [ Minshall , 1960 ; Wang et al. 1981 ]. second Huang Willgoose 1993 Goodrich 1997 ] catchment statistical property, mean annual flood, area catchment. They are both linked important interconnected hydrologic concepts,...
A space‐time rainfall model is constructed to generate synthetic fields of rainfall, with a daily time step. The has two components: temporal based on first‐order, four‐state discrete Markov chain which generates series the regionally averaged and spatial nonhomogeneous random cascade process disaggregates above amounts produce patterns across region. generators used disaggregate spatially are product stochastic deterministic factors; latter enable capture systematic gradients exhibited by...
Assessment of rainfall-induced shallow slope failures is important for reducing damage to infrastructures as well the safety people living close hazardous areas. The rainfall intensity-duration thresholds initiation failure (ID thresholds) based on historical data are commonly used assess failure. However, in these slope-stability assessments, critical influence factors triggering often disregarded. Three sets parametric studies were performed through finite-element modeling investigate...
Understanding the hydrological and physical responses of shallow slopes subject to rainfall events is vital for efficiency a warning system setup. In this research, series experiments were undertaken evaluate varying steepness when subjected intensities, periods, inter-storm periods rainfall. An analysis infinite was also develop fundamental understanding rainfall-induced slope failure characteristics. The characterized in infiltration saturation phases. During phase, maximum magnitude water...
Marginal soils, which possess suitable mechanical properties but fail to meet the fine particle content and plasticity index requirements for stabilised earth (MSE) walls, are of particular interest construction industry as a potential replacement granular backfill materials. A numerical analysis unsaturated flow was conducted assess impact each parameter on hydrological conditions in an MSE wall with geocomposite. The studied results indicate that using marginal soil material widespread...
Water loss from broken or leaking pipe networks is still a major water management problem for the Provincial Waterworks Authority (PWA) in Thailand. To reduce this and benefit savings, district metering area (DMA) was applied as measure to control losses at PWA Lop Buri Branch. The DMA divided into 8 zones, covering about 60.47 % of total service area. A surveillance system set up that compared observed flow rates upper limit warning values each DMA. Comparison results before after...
Download This Paper Open PDF in Browser Add to My Library Share: Permalink Using these links will ensure access this page indefinitely Copy URL Dominant Runoff Response and Travel Time Distribution of Behavioural Catchments 1 Pages Posted: 24 Feb 2024 See all articles by Chatchai JothityangkoonChatchai JothityangkoonSuranaree University TechnologyHaruetai Maskongaffiliation not provided SSRN Abstract The three dominant processes contributing runoff, as proposed the Dunne diagram are...
Development processes of a master plan formulation for flood protection and mitigation consists the selection process targeted area based on risk level, developing present future inundation map identify direction drainage capacity area. Main causes flooding in can be identified leading to designing system both structural non-structural measures, prior public hearing from stakeholders finalize provide maximum benefits less negative impact. These are applied Roi Et Province. Based...
After flood crisis in Thailand 2011, Department of public works and town planning improved the regulation for urban to include protection plan planning. The aim this paper is present an analysis drainage capacity flood-risk areas integrated Sam Khok district, Pathum Thani province. main cause flooding area overbank from Chao Phraya River. topography, climate, hydrological historical data study are collected analysis. Rational method used analyze 12 canals total 87 by using design rainfall...
The three dominant processes contributing to runoff as proposed by the Dunne diagram are Hortonian overland flow (HOF), (DOF) and subsurface storm (SSF). Using a theoretical perspective, we investigate impact of climate, soil, topography vegetation on catchment water balance probability distribution travel times each generation component in respect connected instantaneous response function (CIRF) including interaction partial area connecting outlet. A simple distributed hydrologic model is...