Martin Kočárek Czech University of Life Sciencieas Prague Faculty of Agrobiology Food and Natural Resources Department of Soil Science and Soil Protection.

Slides:



Advertisements
Similar presentations
Particle size Ions  molecular clusters  nanocrystals  colloids  bulk minerals Small particles can have a significant % of molecules at their surface.
Advertisements

Complexes Complex – Association of a cation and an anion or neutral molecule All associated species are dissolved None remain electrostatically effective.
Lecture 20. Adsorption Phenomena
Soil Fertility and Nutrient Bioavailability Sponsored by the DEST program China Higher Education Strategic Initiatives © The University of Adelaide.
1 Factors Influencing the Activity of Foliar and Soil Applied Herbicides.
6.i. Modelling environmental processes: kinetic and equilibrium (quasi-thermodynamic) modelling 6(i)
Class evaluations.
Gas/Particle Partitioning. Why is gas/particle partitioning important? Dispersion of Pollutants Introduced into the Atmosphere as Determined by Residence.
Soil Chemical Properties
Lecture 3. Adsorption on the interphase of liquid-gas Prepared by PhD Falfushynska Halina.
Sorption of Anions Important because: Several nutrients and agricultural chemicals are negatively charged. –Nitrate, phosphate, sulfate, selenate,… Tropical,
Environmental Processes Fundamental processes in soil, atmospheric and aquatic systems 2.i Ion exchange.
The Structures of Magmas No Phase Diagrams!. The Structures of Magmas Melt structure controls: The physical properties of magmas The chemical behaviour.
Paper and Thin layer Chromatography
Soil Sorption Properties Ability of soil to bind various substances from the dispersion medium Polydisperse system is a mixture of particles of various.
LECTURE 10 Introduction to some chemical properties of soils : Factors affecting plant growth (2)
E NVIRONMENTAL CHEMISTRY E 12. water and soil. W ATER AND SOIL Solve problems relating to the removal of heavy- metal ions, phosphates and nitrates from.
Soil Colloids, the final frontier Measuring CEC; sorption concepts; environmental implications.
Conservative and Reactive Solutes Conservative do not react with soil / groundwater Chloride is a good example Sorbed onto mineral grains as well as organic.
Calculating wet topsoil pile weight Calculate the moisture content (w): w = [(g water) / (g dry soil)] x 100 = % Calculate dry topsoil weight using Db.
Ch. 4 continued Soil Properties.
Introduction to GW contamination and
IS SOLUBILITY THE ONLY CONTROL ON SOLUTE CONCENTRATIONS? The answer is NO! Solubility often controls the concentrations of major solutes such as Si, Ca,
Caveats – don’t give K d more power than it deserves Kp and Kd are partitioning and distribution coefficients that vary with soil properties, solution.
Chapter 6 Weathering and Soil
CE 510 Hazardous Waste Engineering
Environmental Factors That Influence Herbicide Performance Dr. Eric P. Prostko Extension Weed Specialist University of Georgia Tifton.
X-Ray Diffraction for Soils
Environmental chemistry
Adsorption Equilibrium Adsorption vs. Absorption –Adsorption is accumulation of molecules on a surface (a surface layer of molecules) in contact with an.
Organic Matter. 1.Aluminosilcates are composed of two fundamental units: silica tetrahedra and aluminum octahedra to form sheet-like structures. 2. Cation.
Chemical Weathering. I. Introduction Chemical Weathering I. Introduction II. Process of Decomposition A. Overview: Decomposition alters minerals into.
Environmental Processes Partitioning of pollutants 3.i Sorption involving organic matter (between air/soil and water/soil)
Chromatography Separates components in mixture: Based on - polarity
Fundamental processes in soil, atmospheric and aquatic systems 2(ii) Partitioning.
1 The Turtle by Ogden Nash Ogden Nash The turtle lives 'twixt plated decks Which practically conceal its sex. I think it clever of the turtle In such a.
Partitioning of pollutants
Surveillance monitoring Operational and investigative monitoring Chemical fate fugacity model QSAR Select substance Are physical data and toxicity information.
A unifying model of cation binding by humic substances Class: Advanced Environmental Chemistry (II) Presented by: Chun-Pao Su (Robert) Date: 2/9/1999.
Chapter 10 - Soil Fertility. Essential Plant Nutrients - 14 are Mineral Based Macros - N, P, K, Ca, Mg, S Micros - B, Cu, Cl, Fe, Mn, Mo, Zn, Ni.
Phase Interactions Objective –to understand the chemical principles, significance and application of Phase changes in Environmental Engineering. Phase.
The Nature of Solubility Structure of Water Properties of Solutions Factors Affecting Gas and Solid Solubility.
Phosphorus Retention Capacity of a Pilot Stormwater Treatment Area in the Lake Okeechobee Basin Y. Wang 1, K.R. Reddy 1, V. Nair 1, O. Villapando 2, and.
Environmental Processes Partitioning of pollutants 3.ii Sorption involving inorganic matter (between air/soil and water/soil)
Aquatic Chemistry 367 Civil and Environmental Engineering Meeting time: MWF 11:00-11:50am Meeting room: Abbott Auditorium in Pancoe Pavillion Instructor:
Ch. 4 continued Soil Properties.
Concepts in Environmental Behavior of Trace Metals 1. CHEMICAL KINETICS AND SORPTION: A REVIEW.
PART -III Analytical Methods for Metal Speciation in Water and Solids
Effectiveness and mechanisms of mercury sorption by biochars from invasive Brazilian pepper at different temperatures Xiaoling Dong 1, Lena Q Ma 1*, Yingjia.
By- Bhavya, Harsh, Harshvardhan, Namrata, Ronit and Vidhatri
The Nature of Solubility
Solubility (cont.); Mineral Surfaces & Reactions Lecture 22.
Soil Acidity and Review of Colloid Charge. Mineral Charge.
Soil colloids. CHEMICAL PROPERTIES OF SOIL: Soil Colloids cat ion Exchange organic matter / Organic carbon Carbon –Nitroge ratio Soil fertility Soil reaction.
Soil Sorption Properties Ability of soil to bind various substances from the dispersion medium Polydisperse system is a mixture of particles of various.
INTRODUCTION Cd Usually it combined with other elements such: oxygen, chlorine, or sulfur. Cd 2+ activities in soils is about M. levels of Cd in.
What Is Soil? Chapter 1. Soil Analysis Ch Why Study Soil Science?  what we call soil is also known as the ‘lithosphere’  it plays an significant.
SOIL FERTILITY.
WATER ACTIVITY μwfood= μwvapor
Soil Chemistry.
SEPARATION METHODS OF ANALYSIS (CHM 703)
Soil Science & Management, 4E
Basic Soil-Plant Relationships
Solubility (cont.); Mineral Surfaces & Reactions
Basic Soil-Plant Relationships
Solid-Water Interface
Specify domain’s starting fluid composition on the Initial pane
Chemical Weathering SAPROLITE.
General form of the ADE:
Mathematical modeling techniques in the engineering of landfill sites.
Presentation transcript:

Martin Kočárek Czech University of Life Sciencieas Prague Faculty of Agrobiology Food and Natural Resources Department of Soil Science and Soil Protection

Introduction Pesticides are significant tools to achieve high and quality harvest The application can bring some risk like soil, water, plants and animals contamination An ideal pesticide has to stay in the soil just for the time which is necessary to reduce weeds, but not longer for his residues to affect consequent growth To decrease a risk accompanied by pesticides application we try to model their movement and degradation by prediction models

The main processes involved in pesticides behaviour before their entrance to the soil Photodecomposition Transport in the air Adsorption by plant leafs

The main factors affecting pesticides behaviour after their entrance to the soil Pesticides undergo many transformation and transportation processes Ratio among liquid, solid and gaseous phases Availability of applicable reactants Physical-chemical properties of soil Physical-chemical properties of pesticides

The main factors involved in pesticides behaviour after their entrance to the soil Climatic conditions Simple degradation processes like hydrolysis and oxidation Composition and activities of microorganisms

The main factors involved in pesticides behaviour

Soil temperature and soil moisture

Pesticide Sorption absorption - sorption (penetration into) a 3D matrix adsorption – sorption to a 2D surface Sorbate: the molecule ad- or absorbed Sorbent: the matrix into/onto which the sorbate ad- or absorbs Ability of soil to bind various substances from the dispersion medium

Pesticide Sorption sorption affects transport: generally, molecules which are sorbed are less mobile in the environment sorbed molecules are not available for phase transfer processes (air-water exchange, etc) and degradation: sorbed molecules are not bioavailable sorbed molecules usually shielded from UV light (less direct photolysis) sorbed molecules cannot come into contact with indirect photoxidants

Pesticide Sorption Mineral Colloids –C–Clay minerals –P–Primary silicates –I–Insoluble phosphates of Al, Fe –P–Polymeric silicic acids (H 2 SiO 3 ) –H–Hydrated oxides (Al, Fe, Mn), sesquioxides Organic Colloids –H–Humic substances –P–Protein, lignin Combined Colloids – Organo-mineral complexes

Electronegative – ACIDOIDS –N–Negatively chargedX-H………H + –A–Adsorption of cations –(–(Clay minerals, humic substances, H 2 SiO 3 ) → most of the soil colloids Electropositive – BASOIDS –P–Positively charged X-OH………OH - –A–Adsorption of anions –(–(hydrates of sesquioxides) Ampholyte – AMPHOLYTOIDES –(–(hydrated polymers of sesquioxides) Soil Coloides

Pesticide Sorption Permanent –i–isomorphic substitutions in the crystal lattice of clay minerals –O–Octahedron : Al 3+ → Fe 2+, Tetrahedron: Si 4+ → Al 3+ Variable –p–pH-dependent charge –I–Is formed by the dissociation of carboxyl groups –n–negative charge increases with increasing of soil pH Origin of Soil Colloid Charge

Evaluation of Sorption Freundlicha equation: S = amount of organicall chemicals adsorbed into weight unit of the soil K f and n = empirical constant C = equilibrium concentration of organic chemicals in soil solution Langmuir equation: S= amount of organicall chemicals adsorbed into weight unit of the soil C = equilibrium concentration of organic chemicals in soil solution K 1 = adsorption constant related to bond strength S max = maximum of adsorbed chemicals

Pesticide Sorption Pesticide The structural formula Molecular weight Solubility in water [µg.L -1 ] KOCDT50GUS = log(DT 50 ) × (4 - log(K oc )) Chlorotoluron 212, ,76 Metribuzin 214, ,88 Prometryn 241,3736, ,83,18 Terbuthylazin 229,78,522586,53,19 Tested Pesticides

Pesticide Sorption Tested Soils

Pesticide Sorption Tested Soils SoilLocationpH KCl Cox (%) CEC (mmol+/100g) Clay (%) Greyic Phaeozem - Loess Čáslav6,531,3529,7513,4 Haplic Chernozem - LoessPraha -Suchdol7,212,0126,3819,3 Arenosol Epieutric -SandSemice5,740,669,133,5 Haplic Cambisol - GneissHumpolec4,371,6326,009,9 Haplic Chernozem - LoessIvanovice na Hanné6,281,7727,1311,4 Haplic Cambisol - QuartziteJince4,991,6123,6320,3 Arenic Chernozem - Grevel sandVleké Chvalovice6,940,9214,136,4 Stagnic Chernozem Siltic - MarliteMilčice7,432,9240,3815,8 SandPolabí8,110,025,633,3 Haplic Cambisol - SyenitePředbořice5,031,7122,884,8 Haplic Luvizem - LoessHněvčeves5,631,0324,0013,9 LoessPraha - Suchdol7,400,4424,1324,5 Dystric Cambisol - GneissVysoké nad Jizerou4,792,3128,4216,9

Pesticide Sorption-Detected values of Freundlich equation parameter (K f ) Soil / SubstrateChlorotoluron K f for n=1.2 Metribuzin K f for n=1.31 Prometryn K f for n=1.17 Terbuthylazin K f for n=1.21 Greyic Phaeozem - Loess 3,340,78433,66632,9496 Haplic Chernozem - Loess 4,641,02844,26913,5284 Arenosol Epieutric - Sand 2,190,3643,86662,6979 Haplic Cambisol - Gneiss 3,73110,81165,7823,4749 Haplic Chernozem - Loess 4,07380,90454,14313,1247 Haplic Cambisol - Quartzite 3,91292,76396,91623,9737 Arenic Chernozem - Grevel sand 2,16730,42382,54022,5067 Stagnic Chernozem Siltic - Marlite 11,8941,30766,51394,7802 Sand 0,46140,08671,20291,214 Haplic Cambisol - Syenite 4,40864,528,02894,7937 Haplic Luvizem - Loess 2,70820,63943,87912,9095 Loess 0,84670,17171,08270,9133 Dystric Cambisol - Gneiss 7,4971,552811,3786,3507

Pesticide Sorption -Adsorption Isotherm Haplic Cambisol Dystric Cambisol Haplic Luvisol Chlorotoluron sorption in laboratory and fild conditiones

Pesticide Sorption -Adsorption Isotherm

Pesticide Sorption Pedotransfer rules Using the regression analysis were evaluated pedotransfer rules for individual pesticides for prediction of Freundlich equation parameter (K f ) at a constant value of parameter n PesticideRegression equationeR2R2 p Chlorotoluron Kf = -0,91 + 2,01*humus [%] 85,60,0000 Metribuzin Kf = 1,74 + 0,28*humus [%] - 0,24*pH_KCl 58,80,0118 Prometryn Kf = 9,51+ 1,24*humus [%] - 1,24*pH_KCl 80,40,0003 Terbuthylazin Kf = 4,36+ 1,16*humus [%] - 0,38*pH_KCl - 0,006*KVK [mmol.kg -1 ] 89,3 0,0001

Maps of Kf coefficient of different pesticides

Pesticide degradation The change of pesticide concentration is described by following equation: Where: c = concentration t = time k r = constant of reaction n = order of reaction

Pesticide degradation Zero order: n=0 First order: n=1 Second order: n=2

Pesticide degradation - Afect of soil horizon, soil moisture and soil temperature Tab. 3: Chlorotoluron half life (DT 50) under the laboratory conditions. Tab. 4: Analysis of Variance for half life (DT 50) - Type III Sums of Squares

Tab. 2: Chlorotoluron half life (DT 50) under the field conditions. Pesticide degradation - Affect of repeated application

Pesticide degradation - Affect of growth

Pesticide degradation - Affect of shading geotextile 0-5 cm

Pesticide Presistence Definition: The ability of a chemical to retain its molecular integrity and hence its physical, chemical, and functional characteristics in the environment through which such a chemical may be transported and distributed for a considerable period of time. (Source: GILP96) Persistence is evaluated using DT-50 or DT-90. Time for disappearance of 50% or 90% the chemical (days).

Pesticide Presistence

Pesticide Transport Capacitive equation: The movement of water between the horizons is derived from the retention capacity of soil Richards equation :  = volumetric soil water content [L 3 L -3 ] t = time [T] H = the total potential [L] K(h) = unsaturated hydraulic conductivity[LT -1 ] x, y, z = coordinate axes [L] vx, vy, vz = flow rate of water [LT -1 ] The movement of water in the soil

Pesticide Transport Substances dissolved in water are transported by convection and hydrodynamic dispersion Convection equation : Dispersion equation : Convective-dispersive equation : q a = advection flow [ML -2 T -1 ] c = concentration of the solution [ML -3 ] v = fluid velocity in the soil[L -1 T -1 ]. q d = flow caused by hydrodynamic dispersions[ML -2 T -1 ] c = concentration of the solution [ML -3 ], D = hydrodynamic dispersion [L 2 T -1 ]

Chlortoluron concentration in each sampled position 35 day after herbicide application Haplic CambisolHaplic Phaeozem

Average chlortoluron concentration detected 35 days after herbicide application

Average chlortoluron concentrations in Days148 Days 35 Days

Comparision of measured and predicted values of chlortoluron concentration in soil

Thanks for Your Attention