2.1. Research Areas
The research focuses on the development and application of Planning and Decision Support Tools to improve the IWRM in three different regions of Vietnam: the upper Dong Nai river basin (Province Lam Dong), the Red River sub basin (Province Nam Dinh) and the Mekong sub basin (City Can Tho; see
Figure 1). These provinces are located in very different natural and geographical settings and represent the diversity of Vietnamese nature, people and economy.
The province of Lam Dong is located in the southern part of the central highlands. Dalat, the provincial capital has 190,000 inhabitants and is located 1,500 m above sea level in the northeast of the province. Lam Dong is characterized by several high plateaus with fertile soils. Main cultivation products besides coffee and tea are cashew nuts, mulberries, flowers, vegetables and fruit. Altogether a surface of 279,000 ha is under cultivation. A large proportion of the province is covered by forest.
Nam Dinh is a coastal province in the southern Red River delta in the northeast of Vietnam. It covers an area of 1,700 km2. The topography of Nam Dinh province is characterized by lowland features. It lowers gradually from northwest to southeast. The province can be divided into two regions: the polder area of the low delta plain (the lowest point is 3 m below sea level), and the coastal plains outside the sea dyke. There are a few hills in the northwestern part of the province (the highest is Goi at 122 m elevation). The coastline has a length of 72 km, but it is extensively separated by large river mouths. The main agricultural product is rice. Furthermore there are more than 100 trade villages—many of them specialized in handicraft production—in Nam Dinh.
Can Tho City is the center of the Mekong Delta. The city is located 135 km southwest of Ho Chi Minh City. The total area of Can Tho is 1,401 km2 and is divided into four urban districts and four mainly rural districts. Can Tho is situated on the Hau River, which is a southeastern distributary of the Mekong River. The Mekong Delta is dominated by agricultural land use. About 50% of the national rice production is generated in the Mekong Delta. About 84% of the area in Can Tho is used for agriculture, more than 90% of it for rice production. Besides this, plant production, aquaculture and animal husbandry have become more and more important.
Figure 1.
Overview of the research area.
Figure 1.
Overview of the research area.
2.2. Concept of the Project
The research project IWRM-Vietnam develops Planning and Decision Support Tools for IWRM especially for Vietnamese conditions. It is based on the following planning levels (
Figure 2). The project is carried out on the planning level of river basins.
- (1)
International level (international guidelines: e.g. Global Water Partnership, Agenda 21)
- (2)
National planning level (national Vietnamese water and environmental policy, national Vietnamese legislation)
- (3)
River basin planning level
- (4)
River sub basin planning level (WMUs)
- (5)
Local sites planning level (local measures)
Figure 2.
Planning levels of the research project IWRM-Vietnam.
Figure 2.
Planning levels of the research project IWRM-Vietnam.
On the river basin planning level (project level of IWRM-Vietnam) the decision relevant information for identification of WMUs (Water Management Units) with priority need for action was recorded. WMUs are sub basins of a river basin that are defined for the purpose of IWRM in the river basin.
The methodical concept consists of three main tools (
Figure 3):
- -
Water Balance Tool: Evaluation of water demand versus water resources;
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Contamination Risk Tool: Evaluation of sensitivity of water resources versus contamination potential;
- -
Ranking Tool: Assessment of WMUs with priority need for action.
Figure 3.
Framework for the Planning and Decision Support tools.
Figure 3.
Framework for the Planning and Decision Support tools.
The Planning and Decision Support Tools are a dynamic approach for the analysis of diverse input data. Due to restricted data availability, the current state of the water demand calculation covers the year 2005 and the water resource is calculated for a year with average rainfall (2002). Due to general data availability and quality in Vietnam being poor, missing water-related issues (e.g., flood modeling, biodiversity conservation, etc.) are planned to be integrated into the methodical IWRM concept in the future by creating an additional thematic database. Only currently available data are considered within the IWRM Vietnam project.
The Planning and Decision Support Tools are applicable for different periods of consideration allowing the implementation of scenarios. Changes of the boundary conditions (e.g., population, climate, economy, land use) allow for a quick and easy derivation of new results.
The visualization of all input components and the results of the three tools take place in a Geographical Information System (GIS). Within the framework of the project, thematic maps with the following themes were developed:
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Basic maps: Water Management Units, administration, population density, land use, orohydrography, natural reserve, geology, soil;
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Water balance: hydrological system, water infrastructure, water resources, water demands, water balance;
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Contamination risk: infiltration into groundwater, diffuse pollution of surface water, direct discharge into surface water.
The following sections outline the application of the method, based on the case study upper Dong Nai river basin (province Lam Dong).
Figure 4 shows the cascade of the WMUs and how they are linked to form a network.
Figure 4.
WMU cascade upper Dong Nai basin (Water Management Units: DN 1‑DN 17, LN 1‑LN 4, TA 1).
Figure 4.
WMU cascade upper Dong Nai basin (Water Management Units: DN 1‑DN 17, LN 1‑LN 4, TA 1).
2.4. Contamination Risk Tool
The Contamination Risk Tool is based on the estimation of contamination risks for water resources (groundwater and surface water) as follows:
To analyze the contamination potential on a regional scale, the emitters of pollutants are considered. A detailed observation of specific pollutants cannot be accomplished due to fragmentary databases. Pollutants can affect water resources via three possible contamination paths (
Figure 8):
Infiltration of solute pollutants from diffuse and point sources into groundwater
Transport of pollutants from diffuse sources by erosive runoff into surface water
Direct discharge of pollutants from point sources into surface water
Figure 8.
Contamination paths (path 1: infiltration, path 2: erosive runoff, path 3: direct discharge).
Figure 8.
Contamination paths (path 1: infiltration, path 2: erosive runoff, path 3: direct discharge).
Figure 9 shows the interrelation between sensitivity of water resources, the possible causes of contamination potentials, and the resulting contamination risks for all three contamination paths. In view of the large number of thematic maps per research area (
i.e., 15) created within the Contamination Risk Tool, only examples for the Dong Nai river basin are presented within this article. The example shows the method of assessing the groundwater sensitivity, the contamination potential and the contamination risk of settlements.
Figure 9.
Aggregation of sensitivity of water resources and contamination potential to contamination risk.
Figure 9.
Aggregation of sensitivity of water resources and contamination potential to contamination risk.
The following is an explanation of the method using the example of path 1 (infiltration into groundwater).
The parameters for the determination of the sensitivity of groundwater (path 1), on the river basin scale, are the result of aquifers and groundwater use. Aquifers with a high sensitivity are hard rock with a high productivity or floodplains (
Figure 10: red color, essentially basalt rock). Aquifers with a medium sensitivity are hard rock with a medium productivity (
Figure 10: orange color, essentially sedimentary rock) and those with a low sensitivity are hard rock with low productivity (
Figure 10: green color, essentially granite rock). Regions with groundwater use and a higher relevance for water supply are set to a very high sensitivity
per se (
Figure 10: hatched areas).
Figure 10.
Map of groundwater sensitivity and groundwater use (path 1).
Figure 10.
Map of groundwater sensitivity and groundwater use (path 1).
The contamination potential of settlements is relevant for path 1, because with the exception of one sewage plant in the province capital Dalat, there are no other treatment facilities. Most of the domestic wastewater reaches the groundwater.
Figure 11 shows the density and distribution of settlements within the river basin. A high settlement density (>70 settlement points/km
2) is shown in red, a medium settlements density (31–70 settlement points/km
2) in orange, a low settlement density (5–30 settlement points/km
2) in green, and no settlement contains areas with less than five settlement points/km
2. The distribution of settlements shows areas where domestic wastewater can reach the groundwater. Population data is available on district level only. Therefore, the settlement building data is used to calculate a settlement density map.
Figure 11.
Map of contamination potential of settlements (path 1).
Figure 11.
Map of contamination potential of settlements (path 1).
The aggregation of groundwater sensitivity, and the contamination potential of settlements to contamination risk, is carried out using the aggregation matrix shown in
Figure 12. Its aim is to classify the contamination risk into three general classes (low, medium, high).
Figure 12.
Aggregation of sensitivity of groundwater and the contamination potential of settlements to contamination risk.
Figure 12.
Aggregation of sensitivity of groundwater and the contamination potential of settlements to contamination risk.
The resulting map shows the different contamination risk intensities for groundwater (path 1) caused by settlements (
Figure 13).
Figure 13.
Map of contamination risk settlements (path 1).
Figure 13.
Map of contamination risk settlements (path 1).