Introduction
Field Investigation
Hydrological Modelling
Water Quality Modelling
Conclusion
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Water Quality Modelling of the
East River
Hydrological Simulation Program Fortran (HSPF)
An
empirically-based lumped parameter model, HSPF (Hydrological Simulation
Program Fortran, Bicknell et al., 2001), is employed to predict
water quality of the East River. The emphasis is on key organic
pollutant concentrations of relevance to drinking water quality
(Biochemical Oxygen Demand BOD5, and ammonia nitrogen NH4.
The lower East River Basin (from Heyuan to Qiaotou) is modelled.
The HSPF study area (9630 km2) covers key cities including
Heyuan, Huizhou, Dongguan, Shenzhen, and their associated counties.
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Based on demographic and pollution data in government reports (PRWRPB,
2000; SCIES, 1999), and the use of ¡§export coefficient¡¨ approach (Fok
et al., 2004), the point source (PS), non point source (NPS) and wet
deposition pollution loads (kg/d) from (i) agricultural, (ii) domestic
and (iii) industrial sources can be estimated.

Left: Study
area of the HSPF model: from Heyuan to Qiaotou
Right: Schematization of the HSPF model
Predicted by the HSPF model,
normally both BOD5 and NH4 concentrations are
below the Chinese National Grade II water quality threshold. However, in
recent years, due to the rapid economic and population growth, and the
inadequate sewage treatment in the region, a considerable increase of
pollutant concentration is predicted. There is a sharp increase in
pollutant concentrations when passing from Boluo to Qiaotou. This
phenomenon can be attributed to the tributary Shimahe (lies in sub-basin
11), which enters the mainstream of the East River at Qiaotou.
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Waste Assimilative Capacity
Waste Assimilative Capacity can
be predicted accordingly. In an extremely dry year such as 2005, annual
averaged concentrations of BOD5 and NH4 can reach
3.67 mg/L and 1.14 mg/L respectively, while the corresponding monthly
flow is 114 m3/s. To maintain both BOD5 and NH4
concentration within the Grade 2 limit of the Chinese Government (3 mg/L
and 0.5 mg/L respectively), the minimum streamflow required at Qiaotou
is 267 m3/s.
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Change in
water quality along the mainstream of the East River, 1998 |

Predicted time-series of water
quality (1985-2007) |
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