As the last post of
2015, let’s look into water quality modelling, in this post we are going to
look at the importance of quality modelling and introduce a modelling package.
Importance of
quality modelling
Water availability is
dependent on quality and quantity. During the last decades, the water courses
have been deteriorated due to anthropogenic discharges of nutrients. The
European Directive and the Water Framework Directive both refer to affluent
loads and the problem of eutrophication. Mathematical modelling is a useful
tool to estimate the pollutant loads into an aquatic environment, to establish
relation between what pollutants has what kind of effect on water quality, and
to predict the response of the aquatic environment under different scenarios.
These simulations are useful tools for management as they assist the decision
makers to come up with strategies that considers the basin conditions as well
as what the effects could be in case of accidental discharges (Oliveira et al, 2012).
The quality of the
freshwater is threatened by population growth, development and expansion of
agricultural and industrial activities, and changes in hydrological cycle as a
result of Climate Change. The water scarcity hand in hand with decreasing water
quality has forced the countries to look into remediation options for river
water quality, and hence effective water management strategies to ensure
sufficient water supplies with high quality is required (Vieira et al,2012).
QUAL2K
QUAL2K is water
quality model for rivers and streams. The model includes many elements such as considering
a one dimensional model, assuming the channel is well-mixed both laterally and
vertically, assuming steady state, non-uniform for flow hydraulics, heat
budgets, and water-quality kinetics that are dependent on heat and mass inputs (Chapra, Pelletierand Tao,
2012).
The model divides the
river into smaller sections of “reaches” and “elements”. Reaches represent a
length of the river with constant hydraulic characteristics such as slope,
bottom width etc. Then each reach can be divided into smaller equally-spaced
units called “elements”. The model’s computations are carried out for each
element. Then flow balance calculations are carried out for each element by
considering a steady-state flow balance equation, then considers the hydraulic
characteristics and the presence of weirs. Each element is then considered as
an idealized trapezoidal channel and uses the Manning Equation to express the
relationship between flow and depth (which we will not get into because I
enjoyed other subject more than fluids dynamics!). The model also has a
temperature model component and calculates the net absorbed radiation as well.
Then the mass balance and flow biochemical reactions are calculated (Chapra,Pelletier and
Tao,2012).
In order the get the
correct result, a series of computations should be done since they are
interdependence. Meaning that a variable such as surface mass transfer
coefficient (s) depends on another variable (SOD), which itself is dependent on
ammonium and methane concentrations, and so on. Hence, an iterative technique
is used in QUAL2K to calculate the fluxes of nitrate, ammonium, and methane,
etc. (Chapra, Pelletier and
Tao,2012).
Pretty complicated
modelling package! It has integrated different fields of water chemistry, fluid
dynamics and fluid thermodynamics! Join me in 2016, where I will look into some
case studies that have used this package and the results they got!
Wishing you all a
fantastic year ahead!
So long,






