Point Propagation Model of Pollution Sources of Heavy Metals in the Surface Soil

Similar documents
Experimental Analysis on Soil-Water Characteristic Curve of CH3COO - Contaminated Clay

RADIONUCLIDE DIFFUSION IN GEOLOGICAL MEDIA

A Hybrid ARIMA and Neural Network Model to Forecast Particulate. Matter Concentration in Changsha, China

1D Verification Examples

The thermal conductance of collection tubes in geothermal energy systems

Heat Conduction in 3D Solids

SAFETY ASSESSMENT CODES FOR THE NEAR-SURFACE DISPOSAL OF LOW AND INTERMEDIATE-LEVEL RADIOACTIVE WASTE WITH THE COMPARTMENT MODEL: SAGE AND VR-KHNP

Numerical Solution of the Two-Dimensional Time-Dependent Transport Equation. Khaled Ismail Hamza 1 EXTENDED ABSTRACT

WASTE MANAGEMENT GLOSSARY

IONIC MIGRATION IN FROZEN SOILS AND ICE

The Mathematical Analysis of Temperature-Pressure-Adsorption Data of Deep Shale Gas

POINT SOURCES OF POLLUTION: LOCAL EFFECTS AND IT S CONTROL Vol. II - Contaminant Fate and Transport Process - Xi Yang and Gang Yu

Mixtures & Solutions. What is matter? What is a mixture? What is a mechanical mixture? What is a solution? What is a pure substance?

Safety assessment for disposal of hazardous waste in abandoned underground mines

Shirley E. Clark, Ph.D., P.E., D. WRE Robert E. Pitt, Ph.D., P.E., BCEE, D. WRE

Experimental Study on the Cyclic Ampacity and Its Factor of 10 kv XLPE Cable

Computational fluid dynamic modeling of Nickel/Metal Hydride (Ni/MH) Battery during Charge Cycle

On the Early Development of Dispersion in Flow through a Tube with Wall Reactions

Thermal and hydraulic modelling of road tunnel joints

The distortion observed in the bottom channel of Figure 1 can be predicted from the full transport equation, C t + u C. y D C. z, (1) x D C.

Time Rate of Consolidation Settlement

Adaptability analysis of radiative transport diffusion approximation in planar-graded-index media

Flow and Transport. c(s, t)s ds,

THE APPLICATION OF GREY SYSTEM THEORY TO EXCHANGE RATE PREDICTION IN THE POST-CRISIS ERA

Consolidation properties of dredger fill under surcharge preloading in coast region of Tianjin

WM2012 Conference, February 26- March 1, 2012, Phoenix, Arizona, USA. Permeability Calculation in a Fracture Network

ROTATIONAL STABILITY OF A CHARGED DIELEC- TRIC RIGID BODY IN A UNIFORM MAGNETIC FIELD

DNAPL migration through interbedded clay-sand sequences

What is Chromatography?

Batch Adsorption Test of Phenol on Soils

Two GM (2,1) Improved Model to Predict Air Quality Index Qianwen An

Spatial Distribution of Magnetic Field under Spherical Shell Plasma

Application of the random walk method to simulate the transport of kinetically adsorbing solutes

Comparison of Heat and Mass Transport at the Micro-Scale

Chapter 2 Methods Based on the Absorption of Gamma-Ray Beams by Matter

Diffusion of a density in a static fluid

Grey prediction model-based men s 100m freestyle Olympic Games performance prediction research

RECIPROCAL INVISIBLE CLOAK WITH HOMOGE- NEOUS METAMATERIALS

O.R. Jimoh, M.Tech. Department of Mathematics/Statistics, Federal University of Technology, PMB 65, Minna, Niger State, Nigeria.

THEORETICAL ANALYSIS AND NUMERICAL CALCULATION OF LOOP-SOURCE TRANSIENT ELECTROMAGNETIC IMAGING

WM 00 Conference, February 27 March 2, 2000, Tucson, AZ DIFFUSION COEFFICIENTS OF CRITICAL RADIONUCLIDES FROM RADIOACTIVE WASTE IN GEOLOGICAL MEDIUM

PHYSICAL REVIEW B 71,

Stress and Wear Analysis of the Disc Cutter of Rock Tunnel Boring Machine

Lecture 16 Groundwater:

Deflection. Hai Huang Min

Modeling microlenses by use of vectorial field rays and diffraction integrals

Radionuclide Migration: Prediction Experience

Pseudo-seismic wavelet transformation of transient electromagnetic response in engineering geology exploration

Modelling of Thermal Behavior of Borehole Heat Exchangers of Geothermal Heat Pump Heating Systems

A fast-burning mechanism for magnetic diffusion

Determination of Poisson s Ratio of Rock Material by Changing Axial Stress and Unloading Lateral Stress Test

Radio Propagation Channels Exercise 2 with solutions. Polarization / Wave Vector

Invention of microscopes and telescopes expanded understanding of the Earth revealing new things

Transactions on Ecology and the Environment vol 7, 1995 WIT Press, ISSN

Add-on unidirectional elastic metamaterial plate cloak

Supporting Information

Relationship between the characteristics of cationic polyacrylamide and sewage sludge dewatering performance in a full-scale plant

Building a Robust Numerical Model for Mass Transport Through Complex Porous Media

Curriculum Vitae. Education Background

Adsorption of Humic acid on Powdered Activated Carbon (PAC)

TECHNOLOGIES THAT TRANSFORM POLLUTANTS TO INNOCUOUS COMPONENTS: CHEMICAL AND PHYSICOCHEMICAL METHODS

1. Water in Soils: Infiltration and Redistribution

Code-to-Code Benchmarking of the PORFLOW and GoldSim Contaminant Transport Models using a Simple 1-D Domain

Experimental Research of Optimal Die-forging Technological Schemes Based on Orthogonal Plan

1 of 7 2/8/2016 4:17 PM

Computational modelling of reactive transport in hydrogeological systems

Research Article Finite Element Analysis of Flat Spiral Spring on Mechanical Elastic Energy Storage Technology

Strand Tension Control in Anchor Span for Suspension Bridge Using Dynamic Balance Theory

Center for Orbital Debris Education and Research

7-1 Life Is Cellular. Copyright Pearson Prentice Hall

RATE OF FLUID FLOW THROUGH POROUS MEDIA

Johns Hopkins University Fax: N. Charles Street

932 Yang Wei-Song et al Vol. 12 Table 1. An example of two strategies hold by an agent in a minority game with m=3 and S=2. History Strategy 1 Strateg

Danwei system in China and its impact on the daily life of urban residents after reform

SECM Study of Permeability of a Thiolated Aryl Multilayer and Imaging of Single Nanocubes Anchored to It

PROPERTIES OF MIXTURES. A mixture is a combination of two or more substances that are not chemically combined

Advanced Hydrology Prof. Dr. Ashu Jain Department of Civil Engineering Indian Institute of Technology, Kanpur. Lecture 6

Air Permeability and Acoustic Absorbing Behavior of Nonwovens

Reservoirs and Production

2017 International Conference on Economics, Management Engineering and Marketing (EMEM 2017) ISBN:

Comparison of Heat and Mass Transport at the Micro-Scale

Lecture No 1 Introduction to Diffusion equations The heat equat

Burial Depth of SAM-III Magnetometer Sensors

A Study of Covariances within Basic and Extended Kalman Filters

BME STUDIES OF STOCHASTIC DIFFERENTIAL EQUATIONS REPRESENTING PHYSICAL LAW

Research Article Stabilization Analysis and Synthesis of Discrete-Time Descriptor Markov Jump Systems with Partially Unknown Transition Probabilities

The generation and mobility of colloids in soils Production et mobilité des colloï des dans les sols

The layered water injection research of thin oil zones of Xing Shu Gang oil field Yikun Liu, Qingyu Meng, Qiannan Yu, Xinyuan Zhao

Optimization of a Multi-pendulum Wave Energy Converter

The Divergence Theorem Stokes Theorem Applications of Vector Calculus. Calculus. Vector Calculus (III)

Deep Borehole Disposal Performance Assessment and Criteria for Site Selection

Correlation analysis. Contents

Dynamics and Control of Lorentz-Augmented Spacecraft Relative Motion

Scalar and vector fields

Basic Concepts of Electrochemistry

Study on Acoustically Transparent Test Section of Aeroacoustic Wind Tunnel

Adsorption of Cesium Ion on Various Clay Minerals and Remediation of Cesium Contaminated Soil in Japan

Optimization of DPF Structures with a 3D-Unit Cell Model

1. Introduction. 2. Model Description and Assumptions

Introduction. Statistical physics: microscopic foundation of thermodynamics degrees of freedom 2 3 state variables!

Transcription:

Int. J. Electrochem. Sci., 8 (013) 5153-5160 International Journal of ELECTROCHEMICAL SCIENCE www.electrochemsci.org Point Propagation Model of Pollution Sources of Heavy Metals in the Surface Soil Hai-ming Zhang 1, Hong-gui Deng 1*, Gu Teng-feng 1, Fang Yang 1, Yi Sun 1, Ji-an Duan 1.School of Physics and Electronics, Central South University, Changsha 410083, China.State Key Laboratory of High Performance Complex Manufacturing, School of Mechanical and Elec trical Engineering, Central South University, Changsha 410083, China) * Corresponding author E-mail: denghonggui@163.com Received: 19 January 013 / Accepted: 14 March 013 / Published: 1 April 013 The soil pollution caused by heavy metal is difficult to treat. Many scientists and researchers are focusing on solving the problem in recently years. By probing into the law of diffusion and the law of conservation of mass, we establish the point propagation model of pollution sources of heavy metals and come to the distribution characteristics function of the local area the concentration of heavy metals in soil. Finally, the proposed point propagation model is utilized to establish a method for determining the point pollution sources. Keywords: Law of Diffusion, Law of Conservation of Mass, Point Propagation Model 1. INTRODUCTION With the fast growth of economy and the rapid advance of urbanization and industrialization in the world, the environmental issues have become increasingly prominent. With the growing awareness of environment protection, many researchers have shown great interests on the mechanism of heavy metals pollution, and they have made great efforts to find solutions to mitigate this problem. In recent decades, many of the great achievements of the world were accomplished on the propagation characteristics of the heavy metal pollutants. The propagation characteristics are mainly characterized by the propagation models, which includes analytical models of deterministic solutions (e.g. the convection-diffusion-adsorption model [1], WASP4 water quality model [], migration transformation model [3]) and empirical models of uncertain solutions, (e.g. the stochastic model [4]). In the analytical models, the distribution regularity and characteristics of the concentration of heavy metal element over time and space can be determined by rigorous derivation and proof.

Int. J. Electrochem. Sci., Vol. 8, 013 5154 However, because these models are just conceptual models [5-9], they are generally employed only for theoretical analysis without any practical value. With those necessary parameters such as the permeability of the heavy metal elements, the migration performance, the soil permeability, and the diffusion coefficient [10] are measured accurately. Theoretically these models can be precisely solved. However, these parameters are different in different regions, even for the different soils in the same region, they may vary greatly. In addition, the measurements are too complex and tedious to be applied for engineering application. In the stochastic model, the input parameters are treated as random variables, normal distribution or lognormal distribution is employed to estimate the randomness of the output variables. Because the influencing factors are loosely treated as random variables in this model, the essential characteristics of the heavy metal pollution cannot be reflected, and the error is large. This model can only perform general estimation and analysis. In this paper, the propagation characteristic of solid waste pollution is modeled. Mainly by the soluble metal compound being dissolved in water, the contamination caused by the accumulation and burying of heavy metal contained wastes enter into the soil and spread to the surrounding areas with the water in the soil [11]. Based on the Law of Diffusion and the Law of Conservation of Mass, the point propagation model of pollution sources of heavy metals is built under strict deducing and reasonable assumption. With this model, we can more accurately determine the pollution sources through sampling points, meanwhile, the shortness of analytical model and random model, which are not practical and accurate, will not appear in the proposed model.. PROPAGATION MODEL OF POINT SOURCES OF HEAVY METAL POLLUTANTS In the research of the diffusion of solute,we use the function N(x, y, z, t) to indicate the solute concentration of substance G in the location (x, y, z) and at the time t. According to the Law of Diffusion and the Law of Conservation of Mass, in the infinitesimal period dt, the mass dm which flows through the infinitesimal area ds along the normal direction n is proportional to the derivative N n ds, which can be expressed as: of the concentration along the normal direction of the curved surface dm D( x, y, z) N dsdt n (1) Where D(x, y, z) is called the diffusion coefficient of substance G at the point (x, y, z) in the solution. For an arbitrary closed curved surface in the solution, the region enclosed by it is referred as. The entire mass of G which flows into this closed curved surface from time t 1 to t is defined as

Int. J. Electrochem. Sci., Vol. 8, 013 5155 t N m D( x, y, z) dsdt t () 1 n Where N represents the directional derivative of N along the unit normal direction n of the n surface. The mass of the inflow indicates that the concentration of the substance G in the has changed. In the time interval (t 1, t ), the concentration has changed from N(x, y, z, t 1 ) to N(x, y, z, t ), while the mass of G corresponding to the changed concentration is defined as [ N( x, y, z, t ) N( x, y, z, t )] dxdydz 1 From the Law of Conservation of Mass, we can determine N t D dsdt [ N( x, y, z, t) N( x, y, z, t1)] dxdydz t 1 n (3) Suppose that the element N has second-order continuous partial derivatives about (x, y, z) and a first-order continuous partial derivatives about t. According to Green's Formula, we can put equation (3) into N N N N ( D ) ( D ) ( D ) dt dt dxdydz x x y y z z t t t t1 t1 Exchanging the integral order to determine t t1 N N N N ( D ) ( D ) ( D ) dt 0 t x x y y z z (4) As t 1, t and the region are arbitrary, we can determine N N N N ( D ) ( D ) ( D ) t x x y y z z (5) If the solution is uniform, then D is a constant, that is, N N N N D( ) t x y z (6) If the diffusion occurs in an enclosed thin layer, the diffusion equation is dimension-decreased to be two-dimensional equation, which is expressed as

Int. J. Electrochem. Sci., Vol. 8, 013 5156 N N N D( ) t x y (7) In the moisture-containing porous unsaturated soil, the main migration form of heavy metal pollution is the diffusion in the soil and the migration of soluble heavy with soil moisture[11]("improvement model of coupled transmission process in unsaturated porous media"). In the soil, the diffusion capacity of the non-soluble heavy metal compound and the heavy metal dust particles is very weak, so the impact can be ignored. With the soil layer is deeper, the pore size of soil will be smaller and the soil is mostly clay, which has a strong block to heavy metals [1]("The study of the accommodate block ability of clay to heavy metal pollutant "), that will greatly hindered the diffusion of heavy metal. When certain depth is reached, the vertical proliferation can be ignored. Relative to the entire region, the thickness is so small that the entire area can be regarded as a thin slice. With soluble heavy metal compound treated as the solute, the concentration distribution of the heavy metal pollutant satisfies equation (7) approximately. To solve the equation (7), the initial and boundary conditions are necessary, which are N N N D( ), t x y N( x, y,0) ( x, y), N 0. x y R Where the initial condition ( xy, ) denotes the initial distribution of pollutant concentration and the boundary condition denotes when R large enough, the region outside is almost free from contamination, that is, the pollutant concentration is 0. We use the method of variables separation to solve the partial differential equations. Taking N( x, y, t) T( t) V( x, y) into the above equation first, we can determine V V ' T () t x y DT ( t) V ( x, y), Where is a non-zero constant. Processing separation to get T ' ( t) DT ( t) 0 (8) V x V y V 0 (9)

Int. J. Electrochem. Sci., Vol. 8, 013 5157 From the above, we can determine D t T() t Ae The equation (9) can be rewritten into polar form, which is V 1V 1 V V 0 r r r r (10) Continues using the method of variables separation and taking V( r, ) R( r) ( ) into equation (10), we can determine R r R r ( ) 1 ( ) 1 ( ) ( ) ( ) R( r) ( ) R( r) 0 r r r r (11) The moisture-containing porous unsaturated soil can be seen as the solution of heavy metal pollutant. With the soil properties are similar and the water content is basically the same in some areas, it can be regarded as the homogeneous solution with isotropic. Thus, () and are not associated. With only one variable contained in (), () is a constant. Then the equation (11) can be defused as R( r) 1 R( r) Rr ( ) 0 r r r (1) Taking r as a replacement, equation (11) can be expressed as R( ) R( ) R( ) 0 (13) The solution of the equation (13) is the zero-order Bessel function, that is, ( 1) a R( ) J ( ) m 0 0 m0 ( m!) Taking r / as a replacement contrary to above, it can be expressed as m ( 1) a0 R() r r m ( m!) m0

Int. J. Electrochem. Sci., Vol. 8, 013 5158 Thus the results can be determined as m Dt ( 1) a0 N(, r,) t Ae ( ) r m ( m! ) m0 Where A, ( ), a0 are non-zero constants, therefore the final results can be expressed as N( r, t) Ae ( 1) m Dt r (14) m m0 ( m!) According to the boundary and initial conditions, the constants and A can be determined respectively to obtain the propagation equation of the heavy metal pollutant completely. 3. APPLICATION OF THE MODEL In equation (14), the time variable t is included. However, in general, when a certain region is to be sampled, the sampling interval is so short that we can ignore the difference of sampling moment D t of the respective sampling points, that is, the time variable t and e in the natural equation are both constants. Thus the equation (14) can be expressed as N( r, t) ( 1) m A r (15) m m0 ( m!) Assuming that there is only one source of pollution in the sampled region and the form of pollution is point pollution, prior to the pollution, this region has not been contaminated, or the time interval between this pollution and the last contaminated is long enough to avoid affecting the current pollution dispersion. Thus, the pollution dispersion form in this region greatly conforms to the propagation model proposed in this paper. If the boundary and initial conditions are determined, we can solve equation (15) to draw the unknown variables. In fact, for the time factor is eliminated, the statement of the initial conditions no longer exists. Meanwhile, the initial conditions cannot be obtained because the initial condition is the description of the pollutant concentration of the whole region. The boundary conditions also cannot be determined according to the information of the sampling points because the pollution source is unknown in advance, so the radius R of the region in the equation N N x y R 0 cannot be determined. Although it is impossible to solve this equation, we can get the revelation: we can assume a point (x 0, y 0 ) as the pollution source and N 0 as the concentration, then, A in the equation (15) is equal to N 0. The boundary conditions can be determined by treating those sampling points which are close to the background value of heavy metal elements as the boundary, thereby variable in the formula and the spatial distribution function of the concentration are also determined. We know that the concentration of pollution sources is the largest, which provides reference range when we determine the value of N 0. N 0 should be larger than the

Int. J. Electrochem. Sci., Vol. 8, 013 5159 maximum value of the sampling points, and the upper limit can be assumed based on experience, or it can also be set great sufficiently. For each value of N 0, we can get a different distribution function, which corresponds to the theoretical value of this function according to the coordinates of the sampling points and then calculate the variance of the theoretical value and the actual value. According to the preset scope and the required accuracy, N 0 is traversed to get a minimum variance for the point (x 0, y 0 ). Then, we can identify the minimum variance points, that is, the pollution sources by point traversal. In conclusion, we establish a method to find the pollution sources by the information of sampling points. It should be noted that the above work can be carried out by Matlab. 4. CONCLUSION In the paper, we propose a point propagation model of heavy metals in the soil based on the Diffusion Law and the Law of Conservation of Mass. Three-dimensional point source propagation model is established on the basis of the assumption that soil is isotropic, and then based on the dynamic balance of the elements in the vertical direction, the model is transformed to two-dimensional point source propagation model by dimension reduction. It can be further simplified as twodimensional harmonic equation by the assumption that the concentration change rate is constant or the rate is very slow, thus the distribution law of heavy metals in the soil is obtained. All this extend a method to determine the pollution sources by the information of sampling points. The method is simple and flexible, and is suitable in engineering application. In addition, the accuracy is relatively high by experimental verification. ACKNOWLEDGEMENTS This work was financially supported by Natural Science Foundation of China (Grant Nos. 6117047 and 9113035) and Hunan Provincial Natural Science Foundation of China (Grant No. 11JJ039) and Graduate Education Reform Project of Central South University (Grant Nos. 011jg01 and 011jg46) and supported by the Fundamental Research Funds for the Central Universities of Central South University (Grant Nos.01zzts064). References 1. C. Wei, Y.Yilin, Z.Aiguo, G.Zeshi, Anhui University of Sci and Tec (Natural Science),5(010)98... R.Ambrose,Wool T A,Martin J L, U.S Environmental Protection Agency,1(1988)317 3. H.Yong, L.Yitian, Advances in Water Sci, 5(004)576. 4. S.Hongjian, W.Xuan, C.Yanshan, J.Agricultural.Eng, 6(006)197. 5. J.Donald,O'Connor, J.Environment.Eng,3(1988)51. 6. B.M.Chanpman, O.James Robert, Environmental Sci.Inf, 6(1986)51. 7. D.Mdckay, S.Paterson, M.Joy, Chemsphere,1(1983) 9. 8. C.S James, Environ.Sci.Technol,11(1977)174 9. Huckahle, J.K, Sci.Documentation Publishing House, 6(1977)157. 10. C.Yonggui, Z.Yinsheng, Z.Keneng, D.Feiyue, Rock and Soil.Mec, 1(007)584 11. L.Yaochu, W.Huai, L.Weihua, Environmental Sci, 1(008)51.

Int. J. Electrochem. Sci., Vol. 8, 013 5160 1. C.Chunqi,Hydrogeological.eng, 6(001)10. 013 by ESG (www.electrochemsci.org)