Modeling dispersion dust Aerosol particles monitoring and
evaluation in desert south sahara
MOHAMMEDI FERHAT , HADDAD HANANE, LAGGOUN CHOUKI
Laboratory L.A.R.H.Y.S.S
Laboratory LMSM
University of Biskra, B.P 145 RP 07000, Biskra, ALGERIA
Abstract: This present study is desired to calculate the concentration in horizontal direction of
flow of pollutant. As any mathematical models of natural systems, a climate model is a
simplification. The degree of accepted simplification determines the complexity of the model
and restricts the applicability of the model to certain questions. Hence, the complexity of a
chosen model sets the limitations to its application. The quality of a climate model is not judged
by the mere number of processes considered, but rather by the quality of how chosen processes
and their couplings are reproduced.
Keywords: pollutants, models, advection, simulation
Received: June 12, 2022. Revised: July 15, 2023. Accepted: August 25, 2023. Published: September 18, 2023.
1. Introduction
Much progress has been made in the
monitoring, modeling and prediction of
African desert dust storms. Of particular
importance is the development of integrated
dust-storm monitoring and modeling
systems on the basis of numerical models,
satellite remote sensing, synoptic
observations and GIS (Geographic
InformationSystem) data. This paper has
three main goals:
- To introduce the physical basis and the
mathematical description of the different
components of the climate system and the
derivation of differential equations which
describe the most important climatic
processes?
- To introduce in the numerical solutions of
ordinary partial differential equations using
examples from climate modeling;
- To use and apply Matlab as a
mathematical-numerical tool. In this work
the predictability of atmospheric flow
depends on the current state of the
atmosphere. Predictability can be
determined by integrating an ensemble of
initial conditions that are within certain
predefined bounds. We employ the software
package Matlab for the numerical
simulations in this paper. The feasibility and
effectiveness of the proposed method is
demonstrated by computer simulation.
Some wildlife species require large stretches
of land in order to meet all of their needs for
food, habitat, and other resources. These
animals are called area sensitive. When the
environment is fragmented, the large patches
of habitat no longer exist. It becomes more
difficult for the wildlife to get the resources
they to survive, possibly becoming threatened
or endangered. While environmental
degradation is most commonly associated
with the activities of humans, the fact is that
environments are also constantly changing
over time. With or without the impact of
human activities, some ecosystems degrade
over time to the point where they cannot
support the life that is "meant" to live there.
The modeling of the scattering of the
pollutants in the atmosphere is based on the
resolution of an equation to the partial
derivatives that binds the temporal evolution
International Journal of Chemical Engineering and Materials
DOI: 10.37394/232031.2023.2.5
Mohammedi Ferhat,
Haddad Hanane, Laggoun Chouki
E-ISSN: 2945-0519
37
Volume 2, 2023
of the concentration in one point to the
phenomena of diffusion and transportation
in the atmosphere, the concentration of air
pollutants in the atmosphere is directly
linked to air quality. High ground level air
pollution concentration can affect both the
public’s health and the environment. There
are regulations in many countries that
require the applicant to do an air dispersion
modeling in order to obtain an approval
certificate for building a new facility.
Dispersion models can be used to predict the
cumulative effect of existing and planned
facilities. In order to predict Ground Level
Concentration (GLC) from various sources,
atmospheric dispersion models are essential.
In the setting of the modeling of the
scattering of the pollutants in the atmosphere
it remains to try to solve the equation
diffusion-transportation bound to the
concentrations of pollutants only. To solve
this equation various possibilities offer
themselves based: - on an algebraic
approach, and a numeric approach
In a first time we have, as makes usually
for reasons of calculation capacity,
privileged the algebraic method. This
method consists in replacing the equation to
the partial derivatives that conditions the
distribution of the concentrations by an
algebraic equation in which one takes into
account the phenomena physics of diffusion
and transportation through the intermediary
of coefficients bound downwind to the
distance, the stability and to the conditions
of broadcasts to the air atmosphere. The
method Gaussian is based on the hypothesis
of the stationeries. To introduce in the
numerical solutions of ordinary partial
differential equations using examples from
climate modeling; and, to use and apply
Matlab as a mathematical-numerical tool.
2. Approaches Mathematical
Physical
Atmospheric dispersion modeling refers to
the mathematical description of contaminant
transport in the atmosphere, physical and
chemical processes have to be described by
mathematical terms in the beginning of the
development of a continental air pollution
model [1, 5]. These processes are: horizontal
transport (advection), horizontal diffusion,
chemical transformations in the atmosphere
combined with emissions from different
sources, deposition of pollutants to the
surface, and vertical exchange (containing
both vertical transport and vertical
diffusion). The dispersion models are used
to estimate or to predict the downwind
concentration of air pollutants or toxins
emitted from sources such as industrial
plants, vehicular traffic or accidental
chemical releases. The partial differential
equation to be solved is the classical
advection dispersion equation extended with
source sink terms to account for the sorption
and degradation processes; the advection-
diffusion equation reduces to
(1)
The height difference between the virtual
source and the real source is called the
plume height. Due to the transient
conditions in which the particles is liberated
to the atmosphere, and being the dispersion
a three-dimensional phenomena, transient
results of concentration are generated for a
fixed height plane of interest (z).
The elevation phenomenon occurs as a
function of wind velocity. Consider the
numerical solution of the advection -
dispersion equation assuming that D=0. In
this case there is only advection without any
physical dispersion/diffusion
. .( )u C K c Q R
C
t
International Journal of Chemical Engineering and Materials
DOI: 10.37394/232031.2023.2.5
Mohammedi Ferhat,
Haddad Hanane, Laggoun Chouki
E-ISSN: 2945-0519
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Volume 2, 2023
CC
V
tz



(2)
Explicit finite difference approximation
for
, 1 , , 1,i n i n i n i n
C C C C
V
tz




(3)
Where sub index i refers to node and sub
index n to time (n+1 unknown value and n
known).
The unknown concentration at time level
n+1 can be solved from
(4)
Otherwise R is a nonlinear function of the
solute concentration C.
Equations (1-3), and (3-4) are solved
numerically using the finite difference
method.
3. Approaches Numerical
The main objective of this work is to
calculate the condition of dispersion and
diffusion of pollutants en atmosphere for
case in south Algeria. We consider again the
climate model given by equation (2.1) but
we examine its time dependence. It is clear
that an analytical solution is only possible
for few cases. For this reason, it has to be
solved using a numerical algorithm. Several
types of analytical solutions exist for the
transport/sorption/degradation problem but
they are limited to some special cases.
However, analytical solutions are very
useful tools to verify the accuracy of the
numerical solution methods and test the
correctness of a computer program. Elliptic
PDE’s are equations with second derivatives
in space and no time derivative [2,3]. The
most important examples are Laplace’s
equation, the formulations assume an
equidistant discretization; adjustments are
necessary if the grid’s resolution is spatially
dependent, Is the numerical solution (5-11)
consistent with the analytical solution;
Either to solve the hyperbolic system:
( , ) ( , ) ( , )
ii
i ij j i
j
uu
K x t m x t u f x t
tx


(5)
we didn't suppose here the conservation of
the sign of the characteristic ki(x,t) speed
( , )
i
dx k x t
dt
(6)
Either ((x, t) a point of grid we write the
equations to the differentials that correspond
to him
So ki (x, t)<0 ; one writes, the numerical
solution converges towards the analytical
one.
Therefore we apply a transformation of
variables,
( , ) ( , )
( , ) ( , )
( , )
( , ) ( , ) ( , )
ii
ii
i
ij j i
j
u x t u x t
u x h t u x t
k x t h
m x t u x t f x t


(7)
If ki (x, t) > 0
Using central difference in space, and
forward difference in time we get
( , ) ( , )
( , ) ( , )
( , )
( , ) ( , ) ( , )
ii
ii
i
ij j i
j
u x t u x t
u x t u x h t
k x t h
m x t u x t f x t


(8)
Ui (x,t) the exact solution of the equations
to the partial derivatives that of the
derivatives first and seconds according to
the formula of Taylor
International Journal of Chemical Engineering and Materials
DOI: 10.37394/232031.2023.2.5
Mohammedi Ferhat,
Haddad Hanane, Laggoun Chouki
E-ISSN: 2945-0519
39
Volume 2, 2023
2
2
2
2
( , )
( , ) ( , )
( , ) ( , )
2
( , ) ( , , )
i
ii
ii
ii
u x t
u x t u x t t
u x t n u x t
t
u x t xt
t



(9)
(0 1, )
iconst

,
Hence, it has been shown that the
numerical solution converges towards the
analytical solution
for arbitrarily small Δt
2
( , )
( , ) ( , ) ( , , )
()
i
i i i
i
u x t
u x h t u x t h x t h
x
const
(10)
This is a distinctive feature of the equation
to be solved. Central differences may also
cause general problems in the case, for
example, that periodic solutions with
unluckily chosen time steps should be
calculated.
Fig.1soil map geographic and biodiversity
south- Algeria[8]
4. Simulation
This Simulation was conducted in
MATLAB environment and the results are
presented for the case of three sources
configuration, in work of [4-9] we’ve
considered a single source in a constant
wind. To solve the 2-D governing Euler
equations a code was developed in this
work, with the software MATLAB
7.8.version using the Jameson’s scheme
(Jameson, 1981), which is a finite volume
spatial discretization method with artificial
dissipative term. We still need to include:
Multiple sources (still with constant
emission rate), Time-dependent wind
velocity, not aligned with x-axis, multiple
contaminants. Ultimately, solve the inverse
problem.
The Matlab code used to produce Fig. [2-4]
is given below. The Matlab code used to
solve Eq. (3-6) and Eq. (7-10) analytically
and numerically and plot Figs. 3 and 4 is
given below. The chemical reaction
equations were solved simultaneously with
the governing equations of transport reaction
diffusion in horizontal dispersion. We used
the Scharfetter-Gummel and Galerkin
methods in figure (5-6) for comparison.
International Journal of Chemical Engineering and Materials
DOI: 10.37394/232031.2023.2.5
Mohammedi Ferhat,
Haddad Hanane, Laggoun Chouki
E-ISSN: 2945-0519
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Volume 2, 2023
5
10
15
5
10
15
20
0
20
40
60
80
100
120
x (km)
pollutans concentration as a Function of Distance
y (km)
vertical concentration
10
20
30
40
50
60
70
80
90
100
110
Figure.2.The solution of 3D transport in the
space (x) – time (t) diagram, visualized
-2
-1
0
1
2
-2
-1
0
1
2
-0.5
0
0.5
x
diffusion the different components in 3D
y
altitude
-0.4
-0.3
-0.2
-0.1
0
0.1
0.2
0.3
0.4
-5
0
50
5
10
0
0.2
0.4
0.6
0.8
1
transmittance
diffusion pollutans particles transport
diffusion
Figure.3. the transport equation with
degradation and dimensionless space
variable
-6 -4 -2 0 2 4 6
-6
-4
-2
0
2
4
6
x
y
particle dispersion according to the wind speed
-10 -8 -6 -4 -2 0246810
-10
-8
-6
-4
-2
0
2
4
6
8
10
x
y
dispersion with low wind
Figure. 4. Transport with wind-Decay and
Degradation 2D.
.
0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1
0.65
0.7
0.75
0.8
0.85
0.9
0.95
1
International Journal of Chemical Engineering and Materials
DOI: 10.37394/232031.2023.2.5
Mohammedi Ferhat,
Haddad Hanane, Laggoun Chouki
E-ISSN: 2945-0519
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Volume 2, 2023
0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1
-1
-0.8
-0.6
-0.4
-0.2
0
0.2
0.4
0.6
0.8
1
Distribution verticale d’une concentration en fonction de la distance
Galerkin
Scharfetter-Gummel
décentréeUP-upwind
:
Fig.5 Profiles for fluid phase concentration
in case of transport
0.001
0.001
0.001
0.001
0.01
0.01
0.01
0.01
0.01
0.01
0.01
0.02
0.02
0.02
0.02
0.02
0.02
0.05
0.05
0.05
0.1
x (m)
y (m)
concentration (mg/m3), max = 0.18
0200 400 600 800 1000 1200 1400 1600 1800 2000
-100
-50
0
50
100
150
200
250
300
350
400
Figure: 6 concentration and dispersion as a
function of distance-contour lines
The effects of land pollution can be found
everywhere. Pollutants in the land not only
contaminate the land itself, but also have
far-reaching consequences [6, 9]. There are
a number of reasons that ecosystems [fig.5-
6], degrade over time. While it may not
always be the fault of humans, humans still
need to recognize the extent to which they
rely on the resources that the natural world
provides. In this sense, environmental
responsibility and stewardship are very
much a matter of self-preservation, and are
an integral part of healthy resource
management practices.
5. Conclusion:
When land pollution is bad enough, it
damages the soil. This means that plants
may fail to grow there, robbing the eco-
system of a food source for animals. Eco-
systems may also be upset by pollution
when the soil fails to sustain native plants,
but can still support other vegetation.
Invasive weeds that choke off the remaining
sources of native vegetation can spring up in
areas that have been weakened by pollution.
This Simulation was conducted in
MATLAB environment and the results are
presented for the case of three sources
configuration, in work of references [1-4]
we’ve considered a single source in a
constant wind. We still need to include:
Multiple sources (still with constant
emission rate), Time-dependent wind
velocity, not aligned with x-axis, multiple
contaminants. Ultimately, solve the inverse
problem. The suggested numerical solution
method for combined advection,
dispersion/diffusion and Biodegradation
gives very accurate results when compared
to analytical solutions. Many of the long-
lasting effects of land pollution, such as the
leaching of chemicals into the soil cannot be
easily reversed. The best way to deal with
land pollution is to keep it from happening
in the first place. A further important
motivation for the development and
application of climate models remains the
aim to assess future climate change.
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International Journal of Chemical Engineering and Materials
DOI: 10.37394/232031.2023.2.5
Mohammedi Ferhat,
Haddad Hanane, Laggoun Chouki
E-ISSN: 2945-0519
42
Volume 2, 2023
[3] Dixon, K. R. 1977. “Thermal Plumes
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[8] https://www.google.dz/ cartography
south Algeria desert
[9] By Jared Skye BA Environmental
Science, Causes of Environmental
Degradation,
http://greenliving.lovetoknow.com/Causes_o
f_Environmental_Degradation
Contribution of Individual Authors to the
Creation of a Scientific Article (Ghostwriting
Policy)
The authors equally contributed in the present
research, at all stages from the formulation of the
problem to the final findings and solution.
Sources of Funding for Research Presented in a
Scientific Article or Scientific Article Itself
No funding was received for conducting this study.
Conflict of Interest
The authors have no conflicts of interest to declare
that are relevant to the content of this article.
Creative Commons Attribution License 4.0
(Attribution 4.0 International, CC BY 4.0)
This article is published under the terms of the
Creative Commons Attribution License 4.0
https://creativecommons.org/licenses/by/4.0/deed.en
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International Journal of Chemical Engineering and Materials
DOI: 10.37394/232031.2023.2.5
Mohammedi Ferhat,
Haddad Hanane, Laggoun Chouki
E-ISSN: 2945-0519
43
Volume 2, 2023