Prediction of Phosphorus Concentration in an Unconfined Aquifer Using Visual Modflow
Groundwater as a source of water for municipal, industrial, and agricultural purposes plays a key role in many societies around the world and should be safeguarded against pollution. Nutrients such as phosphorus can be transported to other places by groundwater and has adverse effect on ecosyste...
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Main Author: | |
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Format: | Thesis |
Language: | English English |
Published: |
2009
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Online Access: | http://psasir.upm.edu.my/id/eprint/7351/1/FK_2009_44a.pdf http://psasir.upm.edu.my/id/eprint/7351/ |
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Institution: | Universiti Putra Malaysia |
Language: | English English |
Summary: | Groundwater as a source of water for municipal, industrial, and agricultural
purposes plays a key role in many societies around the world and should be
safeguarded against pollution. Nutrients such as phosphorus can be
transported to other places by groundwater and has adverse effect on
ecosystem of water bodies. Phosphorus causes turbidity in water and
eutrophication in surface water and aquatic situation to terrestrial constantly.
The objective of this study is to predict groundwater flow direction and
spreading of phosphorus in an aquifer located at the Engineering Complex of
the Universiti Putra Malaysia. Fertilizers, as main source of phosphorus were
used before in study area. Also the fertilizers are currently used at an area
located south of the Engineering Complex and it has an adverse effect on
quality of groundwater. Visual MODFLOW, is a powerful software package,
was used to predict the changes of groundwater flow patterns and
concentration of phosphorus for period of 10 and 50 years respectively. These two periods were selected because adsorption and slow movement of
phosphorus in groundwater usually take long time. However, mobility of
phosphorus is resumed as the adsorption capacity of phosphorus in the soil is
reached.
Data from 11 constructed wells within the study area were collected to
determine groundwater level from surface, thickness of geological formation,
and concentration of phosphorus. Groundwater movement direction was
determined by the triangular linear interpolation and the field data obtained
from the observation wells indicate that groundwater flow is from Southeast to
Northwest. The concentration of orthophosphorus, as the dominant form of
phosphorus was measured in laboratory using spectrophotometer. The results
show that concentrations of orthophosphorus in vicinity of the swamp are 0.64
mg/l, and 0.5 mg/l, in the pond is 0.22 mg/l, in western part of the area is 0.13
mg/l and in the center of study area is 0.31 mg/l. These concentrations of
phosphorus in the study area show that the highest concentration occurs in the
swamp and the concentration decreases with distance from the swamp down to
the value of 0.13 mg/l. Visual MODFLOW, which include MODFLOW and
MT3DMS, was employed to predict the direction of groundwater flow and
concentration of phosphorus for periods of 10 and 50 years. During these
periods two types of Constant Head Boundary (CHB) were used. In the first
type, the CHB was placed in the northern part of the area and movement of
groundwater during the prediction periods was implemented without any change in hydraulic head. The result shows that phosphorus does not flow to
the pond but might be transferred out of the study area due to groundwater
flow. In the second type, the CHB was located by the pond to record the fate of
phosphorus whenever water depth in the pond drops two meters. The result
indicates that the pollutant is directly transferred to the pond from the swamp
especially via layer No.2 and this can be related to its high hydraulic
conductivity. Prediction of contaminated groundwater shows that the
concentration of phosphorus increases at the end of prediction period at the
study area and this can be attributed to its migration from the swamp area. |
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