Point of zero charge of soil clays

Size: px
Start display at page:

Download "Point of zero charge of soil clays"

Transcription

1 J. Jpn. Soc. Soil Phys. No. 30, p.++ +2,**. * Point of zero charge of soil clays Katsutoshi SAKURAI* * Faculty of Agriculture, Kochi University, B-,**, Monobe, Nankoku 12-2/*,, Japan Morisaki et al., +33- PZC +332 Mattoson +3-, ph 1 +3/* X X +30* Yoshinaga and Aomine, +30, a, b ; Wada and Greenland, +31* +31* van Raij and Peech +31, +32+ Uehara and Gillman,**+ ph ph Point of zero charge, PZC s * Gouy-Chapman s *,nekt p +, sinh +.+/ z PZC ph n e k T z y sinh x x + + y x PZC ph ph * 12-2/*,,** :

2 12 30,**. +, + PZC ph *./ ph Sakurai et al., +322 PZC. IEP Isoelectric Point : ph s d PZC ph s *, PZNC Point of zero net charge : Wada and Okamura, +32- ph -. PZSE + M KCl, NH.Cl PZSE Point of zero salt effect : ph ph van Raij

3 : 13 - PZC and Peech, +31, PZSE PZNC IEP, s esu g + s * s H s IS s OS s D Sposito, +32+ PZC sd s H IEP Cation Exchange Capacity, CEC ph 1 + M ph ph CEC Sakurai et al., +322 CEC sum of exchangeable bases CEC Al e#ective CEC, ECEC Soil Survey Sta#, +33, +320 ph ph ph ECEC PZNC Sakurai et al., +323 c *.*/ M ph

4 14 30,**. Oxisols low activity clay CEC +0 cmol g clay + ECEC +, cmol g clay + Soil Survey Sta#, +33, + +32, a, b ; Sakurai et al., +322, +323 a, Sakurai et al., +323 b - Al Sakurai et al., +323 c. Sakurai et al., +33* / +33* 0 Sakurai et al., Hydroxyaluminosilicate-Mt Sakurai and Huang, +33/, +330, +332 ; Taniguchi et al., +333,,***,,**+ ; Saha et al.,,**+,,**,,,** ; +332 ; Sakurai et al., +330, +332 ; Ishizuka et al.,,*** ; Kadir et al.,,**+ +33* f Fe Al Ca SiO, Fe Al ph 1 - Ca Iwasaki et al., +331, : + Saha et al.,,**- PZC PZC +30* + Innersphere complex PZC PZC PZC Uehara and Gillman, +32+, PZC +33* - Rhoton et al.,,**- PZC Schwarz et al.,,***

5 : 15. Rashid et al.,,**, / PZC Korah et al.,,**- PZC ph Boisvert et al.,,*** Boisvert, J-P., Persello, J., Foissy, A., Castaing, J-C. and Cabane, B. (,***) : E#ect of surface charge on the adsorption mode of sodium poly (acrylate) on alumina-coated TiO, used as coating pigment. Colloids Surfaces. A :Physicochem. Eng. Aspects, +02 :,21, : p. 1, +32, a : ph *. /- : -*0 -+,. +32, b : /- : -1/ -13. Ishizuka, S., Tanaka, S., Sakurai, K., Hirai, H., Hirotani, H., Ogino, K., Lee, H.S. and Kendawang, J. J. (+332) :Characterization and distribution of soils at Lambir Hills National Park in Sarawak, Malaysia, with special reference to soil hardness and soil texture. Tropics, 2 : Ishizuka, S., Sakurai, K., Sabang, J., Kendawang, J. J. and Lee, H.S. (,***) :Soil characteristics of an abandoned shifting cultivation land in Sarawak, Malaysia. Tropics, +* :,/+,0-. Iwasaki, K., Tsuji, M. and Sakurai, K. (+331) :Fractionation of copper and manganese in agricultural soils near an abandoned copper mine. Soil Sci. Plant Nutr.,.-, +/ Kadir, S., Sakurai, K., Ishizuka, S., Tanaka, S., Kubota, S., Hirota, M., Priantna, S. J. and Juairiah (,**+) : Characteristics of Ultisols under di#erent wildfire history in South Sumatra, Indonesia :I. Physico-chemical properties. Tropics, +* : /0/ /2* : 03 : :., : 31 +*0. Korah, J., Spieker, W.A. and Regalbuto, J.R. (,**-) : Why ion-doped, PZC-altered silica and alumina fail to influence platinum adsorption. Catalysis Letters, 2/ : +,- +,1.,**+ :. pp * Mattoson, S. (+3-,) :The laws of soil colloidal behavior, IX. Amphoteric reactions and isoelectric weathering. Soil Sci., -. :,*3,.*. Morisaki, H., Kasahara, Y. and Hattori, T. (+33-) : The cell surface charge of fast- and slow-growing bacteria isolated from grassland soil. J. Gen. Appl. Microbiol., -3 : 0/ 1.. Rashid, Md. M., Kang, Y. and Sakurai, K. (,**,) : Selenium chemistry in amorphous iron (hydr) oxide-applied soil as influenced by redox potential (Eh) and ph. Soil Sci. Plant Nutr.,.2 :,0+,03. Rhoton, F.E., Romkens, M. J.M., Bigham, J.M., Zobeck, T.M. and Upchurch, D.R. (,**-) :Ferrihydrite influence on infiltration, runo# and soil loss. Soil Sci. Soc. Am. J., 01 : +,,* +,,0. Saha, U.K., Taniguchi, S. and Sakurai, K. (,**+) : Adsorption behavior of cadmium, zinc and lead on Hydroxyaluminium - and Hydroxyaluminosilicate - Montmorillonite omplexes. Soil Sci. Soc. Am. J., 0/ : 03. 1*-. Saha, U.K., Taniguchi, S. and Sakurai, K. (,**,) :Simultaneous adsorption of cadmium, zinc and lead from their mixed solutions on hydroxyaluminum- hydroxyaluminosilicate- montmorillonite complexes. Soil Sci. Soc. Am. J., 00 : ++1 +,2. Saha, U.K., Iwasaki, K. and Sakurai K. (,**-) :Desorption behavior of cadmium, zinc and lead sorbed

6 16 30,**. on hydroxyaluminum- and hydroxyaluminosilicate- montmorillonite. Clays and Clay Minerals, /+ (/) :.2+.3,. Sakurai, K., Ohdate, Y. and Kyuma, K. (+322) : Comparison of salt titration and potentiometric titration methods for the determination of zero point of charge (ZPC). Soil Sci. Plant Nutr., -. : ,. Sakurai, K., Ohdate, Y. and Kyuma, K. (+323 a) : Potentiometric automatic titration (PAT) method to evaluate zero point of charge (ZPC) of variable charge soils. Soil Sci. Plant Nutr., -/ : 23 +**. Sakurai, K., Ohdate, Y. and Kyuma, K. (+323 b) : Factors a#ecting zero point of charge (ZPC) of variable charge soils. Soil Sci. Plant Nutr., -/ :,+ -+. Sakurai, K., Nakayama, A., Watanabe, T. and K. Kyuma (+323 c) : Influences of aluminum ions on the determination of ZPC (zero point of charge) of variable charge soils. Soil Sci. Plant Nutr., -/ : 0, Sakurai, K., Teshima, A. and Kyuma, K. (+33*) : Changes in zero point of charge (ZPC), specific surface area (SSA), and cation exchange capacity (CEC) of kaolinite and montmorillonite and strongly weathered soils caused by Fe and Al coatings. Soil Sci. Plant Nutr., -0 : 1-2,. +33* : ZPC -. :, +.. Sakurai, K., Nakamura, Y. and Kyuma, K. (+33+) : Changes in zero point of charge (ZPC), phosphate retention and specific surface area of some variable charge soils after several chemical treatments. Soil Sci. Plant Nutr., -1 :.-/... Sakurai, K. and Huang, P.M. (+33/) : Chapter.. Cadmium adsorption on the hydroxyaluminummontmorillonite complexes influenced by oxalate. In : P.M. Huang, J. Berthelin, J.M. Bollag, W. B. McGill and A.L. Page (Eds.), Environmental impacts of soil component interactions. Vol. + Lewis Publishers, FL, USA, p Sakurai, K., Kozasa, S., Puriyakorn, B., Preechapanya, P., Tanpibal, V., Muangnil, K. and Prachaiyo, B. (+330) : Mineralogical and physico-chemical properties of four Thai soils with special reference to specific surface area (SSA) and zero point of charge (ZPC). Soil Sci. Plant Nutr.,., : 3- +* :ZPC 01 : -, -3. Sakurai, K. and Huang, P.M. (+330) : Influence of potassium chloride on desorption of cadmium sorbed on hydroxyaluminosilicate- montmorillonite complex. Soil Sci. Plant Nutr.,., :.1/.2+. Sakurai, K. and Huang, P.M. (+332) : Intercalation of hydroxy-aluminosilicate and hydroxy-aluminum in montmorillonite and resultant physicochemical properties. Soil Sci. Soc. Am. J., 0, : -0, -02. Sakurai, K., Tanaka, T., Ishizuka, S. and Kanzaki, M. (+332) :Di#erences in soil properties of dry evergreen and dry deciduous forests in the Sakaerat Environmental Research Station. Tropics, 2 : 0+ 2*. Schwarz, S., Lunkwitz, K., Kessler, B., Spiegler, U., Killmann, E. and Jaeger, W. (,***) : Adsorption and stability of colloidal silica. Colloids and Surfaces A, +0- : +1,1. Soil Survey Sta# (+33,) : Keys to Soil Taxonomy, / th edition. SMSS technical monograph No. +3. Blacksburg, Virginia : Pocahontas Press, Inc. p. //0. Sposito, G. (+32+) : The operational definition of the zero point of charge in soils. Soil Sci. Soc. Am. J.,./ :,3,,31. Taniguchi, S., Hiradate, S. and Sakurai, K. (+333) : Speciation of aluminum in hydroxyaluminum and hydroxyalumino- silicate ions fixed by Mt, using,1al-nmr and ICP-AES. Clay Sci., +* :..-.//. Taniguchi, S., Yamagata, N. and Sakurai, K. (,***) : Cadmium Adsorption on Hydroxyalumino-silicate - Montmorillonite Complex as Influenced by Oxalate and Citrate. Soil Sci. Plant Nutr.,.0 : -+/ -,.. Taniguchi, S., Hiradate, S. and Sakurai, K. (,**+) : Speciation of Hydroxyaluminosilicate and Hydroxyaluminium ions as a#ected by the presence of Montmorillonite : extraction experiment with potassium chloride and speiation by,1 Al-NMR. Soil Sci. Plant Nutr.,.1 :

7 : 17 Uehara, G.. and Gillman, G.P. (+32+) : The mineralogy, chemistry, and physics of tropical soils with variable charge clays. Westview Tropical Agriculture Series, No... Westview Press, Boulder, Colorado. p. +1*. van Raij, B. and Peech, M. (+31,) : Electrochemical properties of some Oxisols and Alfisols of the tropics. Soil Sci. Soc. Am. Proc., -0 : /21 /3-. Wada, K. and Greenland, D. J. (+31*) : Selective dissolution and di#erential infrared spectroscopy for characterization of amorphous constituents in soil clays. Clay Miner., 2 :,.+,./. Wada, K. and Okamura, Y. (+32-) : Net charge characteristics of Dystrandept B and theoretical prediction. Soil Sci. Soc. Am. J.,.- : 3*, 3*/. Yoshinaga, N. and Aomine, S. (+30, a) : Allophane in some Ando soils. Soil Sci. Plant Nutr., 2 : Yoshinaga, N. and Aomine, S. (+30, b) : Imogolite in some Ando soils. Soil Sci. Plant Nutr., 2 : ++. +,+. :,**- +, / :,**. +,0

8 18 30,**. : PZC IEP, PZNC, PZSE + pk : : + pk :

Influences of aluminum ions on the determination of zpc (zero point of charge) of variable charge soils

Influences of aluminum ions on the determination of zpc (zero point of charge) of variable charge soils Soil Science and Plant Nutrition ISSN: 0038-0768 (Print) 1747-0765 (Online) Journal homepage: http://www.tandfonline.com/loi/tssp20 Influences of aluminum ions on the determination of zpc (zero point of

More information

ISSN: (Print) (Online) Journal homepage:

ISSN: (Print) (Online) Journal homepage: Soil Science and Plant Nutrition ISSN: 0038-0768 (Print) 1747-0765 (Online) Journal homepage: http://www.tandfonline.com/loi/tssp20 Changes in Zero Point of Charge (ZPC), Specific Surface Area (SSA), and

More information

Lecture 14: Cation Exchange and Surface Charging

Lecture 14: Cation Exchange and Surface Charging Lecture 14: Cation Exchange and Surface Charging Cation Exchange Cation Exchange Reactions Swapping of cations between hydrated clay interlayers and the soil solution Also occurs on organic matter functional

More information

Acid Soil. Soil Acidity and ph

Acid Soil. Soil Acidity and ph Acid Soil Soil Acidity and ph ph ph = - log (H + ) H 2 O H + + OH - (H + ) x (OH - )= K w = 10-14 measures H + activity with an electrode (in the lab), solutions (in the field) reflects the acid intensity,

More information

Cation Exchange Capacity, CEC

Cation Exchange Capacity, CEC Cation Exchange Capacity, CEC The basic building blocks of clay minerals are: silicon atoms surrounded by four oxygen atoms (tetrahedra), and aluminium atoms surrounded by six hydroxide groups (dioctahedra),

More information

Lecture 15: Adsorption; Soil Acidity

Lecture 15: Adsorption; Soil Acidity Lecture 15: Adsorption; Soil Acidity Surface Complexation (Your textbook calls this adsorption ) Surface Complexation Both cations and anions can bind to sites on the external surfaces of soil minerals

More information

Soil Colloidal Chemistry. Compiled and Edited by Dr. Syed Ismail, Marthwada Agril. University Parbhani,MS, India

Soil Colloidal Chemistry. Compiled and Edited by Dr. Syed Ismail, Marthwada Agril. University Parbhani,MS, India Soil Colloidal Chemistry Compiled and Edited by Dr. Syed Ismail, Marthwada Agril. University Parbhani,MS, India 1 The Colloidal Fraction Introduction What is a colloid? Why this is important in understanding

More information

Lecture 6. Physical Properties. Solid Phase. Particle Composition

Lecture 6. Physical Properties. Solid Phase. Particle Composition Lecture 6 Physical Properties Solid Phase Particle Composition 1 Questions What are tetrahedrons and octahedrons? How do silica tetrahedra bonds affect mineral weathering? Difference between primary and

More information

A few more details on clays, Soil Colloids and their properties. What expandable clays do to surface area. Smectite. Kaolinite.

A few more details on clays, Soil Colloids and their properties. What expandable clays do to surface area. Smectite. Kaolinite. A few more details on clays, Soil Colloids and their properties What expandable clays do to surface area Kaolinite Smectite Size 0.5-5 µm External surface 10-30 m 2 /g Internal surface - Size 0.1-1 µm

More information

Chapter 7: Anion and molecular retention

Chapter 7: Anion and molecular retention I. Anions and molecules of importance in soils Anions of major importance to agricultural soils and soil chemistry are: H 2 PO - 4, HPO 2-4, SO 2-4, HCO - 3, NO - 3, Cl -, F - and OH -. Also, micronutrients

More information

The Geochemistry of Natural Waters

The Geochemistry of Natural Waters The Geochemistry of Natural Waters Surface and Groundwater Environments Third Edition James I. Drever University of Wyoming Prentice Hall Upper Saddle River. NJ 07458 Contents 3 Preface xi 1 The Hydrologie

More information

* Tsado, P. A. 1, A. O. Osunde 1, C. A. Igwe 2, P.C. Eze 1 and E. Daniya 3

* Tsado, P. A. 1, A. O. Osunde 1, C. A. Igwe 2, P.C. Eze 1 and E. Daniya 3 INFLUENCE OF ORGANIC ACIDS ON PHOSPHATE SORPTION AND AVAILABILITY IN AN ALFISOL OF NIGERIAN GUINEA SAVANNA * Tsado, P. A. 1, A. O. Osunde 1, C. A. Igwe 2, P.C. Eze 1 and E. Daniya 3 1 Department of Soil

More information

SOIL and WATER CHEMISTRY

SOIL and WATER CHEMISTRY SOIL and WATER CHEMISTRY An Integrative Approach MICHAEL E. ESSINGTON CRC PRESS Boca Raton London New York Washington, D.C. Table of Contents Chapter 1 The Soil Chemical Environment: An Overview 1 1.1

More information

Adsorption of ions Ion exchange CEC& AEC Factors influencing ion

Adsorption of ions Ion exchange CEC& AEC Factors influencing ion Adsorption of ions Ion exchange CEC& AEC Factors influencing ion exchange- Significance. Adsorption of ions Ion adsorption and subsequent exchange are important processes that take place between soil colloidal

More information

Nanoparticles in Soils

Nanoparticles in Soils Diversity of Natural Nanoparticles in Soils Joe B. Dixon Emeritus Professor of Soil Clay Mineralogy Soil and Crop Sciences Dept. Texas A&M University Ferrihydrite Structure update: Michel, et al., Science

More information

The Lithosphere. Definition

The Lithosphere. Definition 10/14/2014 www.komar.de The Lithosphere Ben Sullivan, Assistant Professor NRES 765, Biogeochemistry October 14th, 2014 Contact: bsullivan@cabnr.unr.edu Definition io9.com tedquarters.net Lithos = rocky;

More information

Soil Solution Concentration Prediction of Volcanic Ash Soil upon Addition of Acid Solutions di#er in Anion Composition

Soil Solution Concentration Prediction of Volcanic Ash Soil upon Addition of Acid Solutions di#er in Anion Composition J. Jpn. Soc. Soil Phys. No. 3-, p.-++,**- * ****** Soil Solution Concentration Prediction of Volcanic Ash Soil upon Addition of Acid Solutions di#er in Anion Composition Kouji KAMEYAMA*, Susumu MATSUKAWA**,

More information

Lecture 6: Soil Profiles: Diagnostic Horizons

Lecture 6: Soil Profiles: Diagnostic Horizons Lecture 6: Soil Profiles: Diagnostic Horizons Complexity in Soil Profiles Soil Horizons Soils display distinct layering O Horizon: Partially decomposed organic matter (OM) A Horizon: Near surface, mineral

More information

Overview. Rock weathering Functions of soil Soil forming factors Soil properties

Overview. Rock weathering Functions of soil Soil forming factors Soil properties UN-FAO A. Healthy soils are the basis for healthy food production. B. A tablespoon of normal topsoil has more microorganisms than the entire human population on Earth. C. It can take up to 1,000 years

More information

Chunmei Chen A,B and Donald L Sparks A. Delaware, Newark, DE 19711, USA.

Chunmei Chen A,B and Donald L Sparks A. Delaware, Newark, DE 19711, USA. Environ. Chem. 2015, 12, 64 CSIRO 2015 Supplementary material Multi-elemental scanning transmission X-ray microscopy near edge X-ray absorption fine structure spectroscopy assessment of organo mineral

More information

Sorption-Desorption at Colloid-Water Interface:

Sorption-Desorption at Colloid-Water Interface: Sorption-Desorption at Colloid-Water Interface: A Phenomenon of Environmental Significance Soil Chemical Processes and Ecosystem Health Soil is THE MOST IMPORTANT sink of contaminants Calculated equilibrium

More information

Effects of phthalic and salicylic acids on Cu(II) adsorption by variable charge soils

Effects of phthalic and salicylic acids on Cu(II) adsorption by variable charge soils iol Fertil Soils (26) 42: 443 449 DOI.7/s374-6-89-2 ORIGINL PPER Renkou Xu. Shuangcheng Xiao. Dan Xie. Guoliang Ji Effects of phthalic and salicylic acids on Cu(II) adsorption by variable charge soils

More information

CLASS EXERCISE 5.1 List processes occurring in soils that cause changes in the levels of ions.

CLASS EXERCISE 5.1 List processes occurring in soils that cause changes in the levels of ions. 5 SIL CHEMISTRY 5.1 Introduction A knowledge of the chemical composition of a soil is less useful than a knowledge of its component minerals and organic materials. These dictate the reactions that occur

More information

The Lithosphere. Definition

The Lithosphere. Definition 10/12/2015 www.komar.de The Lithosphere Ben Sullivan, Assistant Professor NRES 765, Biogeochemistry October 14th, 2015 Contact: bsullivan@cabnr.unr.edu Definition io9.com tedquarters.net Lithos = rocky;

More information

Soil Fertility. Fundamentals of Nutrient Management June 1, Patricia Steinhilber

Soil Fertility. Fundamentals of Nutrient Management June 1, Patricia Steinhilber Soil Fertility Fundamentals of Nutrient Management June 1, 2010 Patricia Steinhilber Ag Nutrient Management Program University of Maryland College Park Main Topics plant nutrition functional soil model

More information

Igneous rocks + acid volatiles = sedimentary rocks + salty oceans

Igneous rocks + acid volatiles = sedimentary rocks + salty oceans The Lithosphere Weathering physical processes chemical processes biological processes weathering rates Soil development soil formation processes types of soils and vegetation soil properties physical chemical

More information

CONTENTS PART 1 - MINERALOGICAL ANALYSIS. CHAPTER 1 Water Content and Loss on Ignition. CHAPTER 2 Particle Size Analysis

CONTENTS PART 1 - MINERALOGICAL ANALYSIS. CHAPTER 1 Water Content and Loss on Ignition. CHAPTER 2 Particle Size Analysis CONTENTS PART 1 - MINERALOGICAL ANALYSIS CHAPTER 1 Water Content and Loss on Ignition 1.1 Introduction...3 1.2 Water Content at 105 C (H 2 O )...6 1.2.1 Principle...6 1.2.2 Materials...6 1.2.3 Sample...6

More information

Pyrite in acid sulfate soils: transformation and inhibition of its oxidation by application of natural materials

Pyrite in acid sulfate soils: transformation and inhibition of its oxidation by application of natural materials Symposium no. 28 Paper no. 97 Presentation: oral Pyrite in acid sulfate soils: transformation and inhibition of its oxidation by application of natural materials SHAMSHUDDIN Jusop and SARWANI Muhrizal

More information

SOIL. The Exciting World Beneath Our Feet. J. Kenneth Torrance Professor Emeritus Geography and Environmental Studies Carleton University

SOIL. The Exciting World Beneath Our Feet. J. Kenneth Torrance Professor Emeritus Geography and Environmental Studies Carleton University SOIL The Exciting World Beneath Our Feet. J. Kenneth Torrance Professor Emeritus Geography and Environmental Studies Carleton University Learning in Retirement, Jan 12 Feb 9, 2015 Outline 1 Intro; Minerals;

More information

CHEMICAL, PHYSICAL, AND MINERALOGICAL PROPERTIES OF CERTAIN SOIL PROFILES IN THE LOWER MISSISSIPPI DELTA B. N. DRISKELL ABSTRACT

CHEMICAL, PHYSICAL, AND MINERALOGICAL PROPERTIES OF CERTAIN SOIL PROFILES IN THE LOWER MISSISSIPPI DELTA B. N. DRISKELL ABSTRACT CHEMICAL, PHYSICAL, AND MINERALOGICAL PROPERTIES OF CERTAIN SOIL PROFILES IN THE LOWER MISSISSIPPI DELTA B. N. DRISKELL Louisiana State University ABSTRACT The soils of the lower Mississippi Delta are

More information

The Lithosphere. Definition

The Lithosphere. Definition 10/23/2017 www.komar.de The Lithosphere Modified lecture of Dr. Ben Sullivan Definition io9.com tedquarters.net Lithos = rocky; Rocky sphere Skin of an apple Two basic types crust: oceanic, continental

More information

Influence of soil type and land use on the nature of mobile colloids: implications for the metal transfer in soils

Influence of soil type and land use on the nature of mobile colloids: implications for the metal transfer in soils Symposium no. 01 Paper no. 1289 Presentation: poster Influence of soil type and land use on the nature of mobile colloids: implications for the metal transfer in soils CITEAU Laëtitia, LAMY Isabelle, van

More information

Chemically Surfaced Modified Zeolites ZMM CSMZ. LuVerne E.W. Hogg ZMM CANADA CORP.

Chemically Surfaced Modified Zeolites ZMM CSMZ. LuVerne E.W. Hogg ZMM CANADA CORP. Chemically Surfaced Modified Zeolites ZMM CSMZ October 1, 2014 LuVerne E.W. Hogg ZMM CANADA CORP. NATURAL MINERAL ZEOLITE The high purity Clinoptilolite zeolite provides an excellent matrix for making

More information

GEOCHEMISTRY, GROUNDWATER AND POLLUTION,

GEOCHEMISTRY, GROUNDWATER AND POLLUTION, GEOCHEMISTRY, GROUNDWATER AND POLLUTION, 2 ND EDITION C.A.J. APPELO Hydrochemical Consultant, Amsterdam, the Netherlands D. POSTMA Environment & Resources DTU, Technical University of Denmark, Kgs. Lyngby,

More information

Chemical Weathering and Soils

Chemical Weathering and Soils Chemical Weathering and Soils Fresh rocks and minerals that once occupied the outermost position reached their present condition of decay through a complex of interacting physical, chemical, and biological

More information

Lecture 13 More Surface Reactions on Mineral Surfaces. & Intro to Soil Formation and Chemistry

Lecture 13 More Surface Reactions on Mineral Surfaces. & Intro to Soil Formation and Chemistry Lecture 13 More Surface Reactions on Mineral Surfaces & Intro to Soil Formation and Chemistry 3. charge transfer (e.g., ligand/donor sorption): Sorption involves a number of related processes that all

More information

Particles in aqueous environments

Particles in aqueous environments Lecture 11 Particle-Aqueous Solute Interactions Today 1. Particle types and sizes 2. Particle charges 3. Particle-solute Interactions Next time Please continue to read Manahan Chapter 4. 1. Fresh-salt

More information

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

Shirley E. Clark, Ph.D., P.E., D. WRE Robert E. Pitt, Ph.D., P.E., BCEE, D. WRE Shirley E. Clark, Ph.D., P.E., D. WRE Robert E. Pitt, Ph.D., P.E., BCEE, D. WRE Current PA Guidance Many guidance documents apply expected pollutant removals based on literature. However, typically presented

More information

Effect of nanoparticle of volcanic ash and rock phosphate on some soil chemical properties of variable charge Andisols, Indonesia

Effect of nanoparticle of volcanic ash and rock phosphate on some soil chemical properties of variable charge Andisols, Indonesia DOI:10.25252/SE/18/51414 Online ISSN: 2075-1141 Print ISSN: 2074-9546 Effect of nanoparticle of volcanic ash and rock phosphate on some soil chemical properties of variable charge Andisols, Indonesia Mahfud

More information

Weathering The effects of the physical and chemical environment on the decomposition of rocks

Weathering The effects of the physical and chemical environment on the decomposition of rocks Weathering The effects of the physical and chemical environment on the decomposition of rocks - Igneous rocks form at high temperatures and the constituent minerals reflect the conditions of formation.

More information

Supporting Information

Supporting Information Supporting Information Chemical speciation of cadmium and sulfur K-edge XANES spectroscopy in flooded paddy soils amended with zero-valent ion Yohey Hashimoto 1), and Noriko Yamaguchi 2) 1) Corresponding

More information

Solapur University, Solapur. Syllabus for B.Sc. II- Geochemistry - (IDS) Semester System - CGPA To be implemented from Academic Year

Solapur University, Solapur. Syllabus for B.Sc. II- Geochemistry - (IDS) Semester System - CGPA To be implemented from Academic Year Solapur University, Solapur Syllabus for B.Sc. II- Geochemistry - (IDS) Semester System - CGPA To be implemented from Academic Year- 2015-16 Course Structure Total Credit 16 - (Theory (4 x 3) = 12+Practical

More information

Lecture 7: Introduction to Soil Formation and Classification

Lecture 7: Introduction to Soil Formation and Classification Lecture 7: Introduction to Soil Formation and Classification Soil Texture and Color Analysis Lab Results Soil A: Topsoil from Prof. Catalano s backyard Soil B: Soil above beach at Castlewood State Park

More information

INTERACTION OF IRON OXIDES WITH CLAYS

INTERACTION OF IRON OXIDES WITH CLAYS Clay Science 7, 227-242 (1989) INTERACTION OF IRON OXIDES WITH CLAYS MASAMI OHTSUBO Department of Agricultural Engineering Kyushu University Fukuoka-shi, 812 Japan (Accepted April 13, 1989) ABSTRACT The

More information

ZINC ADSORPTION BEHAVIOR OF DIFFERENT TEXTURED CALCAREOUS SOILS USING FREUNDLICH AND LANGMUIR MODELS

ZINC ADSORPTION BEHAVIOR OF DIFFERENT TEXTURED CALCAREOUS SOILS USING FREUNDLICH AND LANGMUIR MODELS Pak. J. Agri. Sci., Vol. 45(1), 2008 ZINC ADSORPTION BEHAVIOR OF DIFFERENT TEXTURED CALCAREOUS SOILS USING FREUNDLICH AND LANGMUIR MODELS M.S. Ashraf*, A.M. Ranjha*, M. Yaseen*, N. Ahmad** and A. Hannan***

More information

List of Equipment, Tools, Supplies, and Facilities:

List of Equipment, Tools, Supplies, and Facilities: Unit D: ph of Soil Lesson 2: Identifying ph Connection With Plant Growth Student Learning Objectives: Instruction in this lesson should result in the students achieving the following objectives: 1. Explain

More information

Soil ph: Review of Concepts

Soil ph: Review of Concepts Soils and Water, Spring 008 Soil ph: Review of Concepts Acid: substance that can donate a proton Base: substance that can accept a proton HA H A HA and A - are called conjugate acid-base pairs. The strength

More information

Transformation of short-range order minerals in maize (Zea mays L.) rhizosphere

Transformation of short-range order minerals in maize (Zea mays L.) rhizosphere Plant Soil Environ. Vol. 60, 2014, No. 6: 241 248 Transformation of short-range order minerals in maize (Zea mays L.) rhizosphere D. Chatterjee, S.C. Datta, K.M. Manjaiah Division of Soil Science and Agricultural

More information

Maine Agricultural and Forest Experiment Station

Maine Agricultural and Forest Experiment Station The University of Maine DigitalCommons@UMaine Technical Bulletins Maine Agricultural and Forest Experiment Station 5-1-1979 TB91: The Effect of Acidity, Organic Matter, and Sesquioxide Polymers on the

More information

Examination into the accuracy of exchangeable cation measurement in

Examination into the accuracy of exchangeable cation measurement in Examination into the accuracy of exchangeable cation measurement in saline soils H. B. So 1, N. W. Menzies 1, R. Bigwood 1,2, P. M. Kopittke 1,* 1 School of Land and Food Sciences, The University of Queensland,

More information

organisms CaCO 3 + H 2 O + CO 2 shallow water

organisms CaCO 3 + H 2 O + CO 2 shallow water Weathering and Reverse weathering Step I:Weathering of igneous rocks 1. Igneous rocks are mainly composed of Al, Si and O 2 with minor and varying quantities of Na, K, Ca and Mg composing pheldspar minerals

More information

Environmental Soil Chemistry SOCR Credits (3-0-1)

Environmental Soil Chemistry SOCR Credits (3-0-1) Environmental Soil Chemistry SOCR 567 4 Credits (3-0-1) Professor Dr. Thomas Borch is the instructor for this class. He is a Professor in the Department of Soil and Crop Sciences and in the Department

More information

BUFFERING MECHANISM AND SENSITIVITY TO ACID DEPOSITION OF SOILS OF AKWA IBOM STATE, NIGERIA

BUFFERING MECHANISM AND SENSITIVITY TO ACID DEPOSITION OF SOILS OF AKWA IBOM STATE, NIGERIA BUFFERING MECHANISM AND SENSITIVITY TO ACID DEPOSITION OF SOILS OF AKWA IBOM STATE, NIGERIA ABSTRACT Akpan *, U. S. and Udoh, B. T. Department of Soil Science and Land Resources Management, University

More information

CATION EXCHANGE IN KAOLINITE-IRON

CATION EXCHANGE IN KAOLINITE-IRON CATION EXCHANGE IN KAOLINITE-IRON OXIDE SYSTEMS* by GRANT W. THOMAS and ALLEN R. SWOBODA Virginia Polytechnic Institute, Blacksburg, Virginia ABSTRACT Kaolinite, to which iron oxides had been added by

More information

Copyright SOIL STRUCTURE and CLAY MINERALS

Copyright SOIL STRUCTURE and CLAY MINERALS SOIL STRUCTURE and CLAY MINERALS Soil Structure Structure of a soil may be defined as the mode of arrangement of soil grains relative to each other and the forces acting between them to hold them in their

More information

Molecular Sieves Principles of Synthesis and Identification

Molecular Sieves Principles of Synthesis and Identification Molecular Sieves Principles of Synthesis and Identification Second Edition R. SZOSTAK Clark Atlanta University Atlanta, GA USA V D BLACKIE ACADEMIC & PROFESSIONAL An Imprint of Chapman & Hail London Weinheim

More information

Boron Adsorption by Some Semi-Arid Soils of North Eastern Nigeria

Boron Adsorption by Some Semi-Arid Soils of North Eastern Nigeria International Journal of Applied Agricultural Research ISSN 0973-2683 Volume 6 Number 1 (2011) pp. 71 76 Research India Publications http://www.ripublication.com/ijaar.htm Boron Adsorption by Some Semi-Arid

More information

A horizon. Clay Basics. Clays: A horizon. Phyllosilicates phyllon = leaves. Clay formation. Zone were parent materials weather

A horizon. Clay Basics. Clays: A horizon. Phyllosilicates phyllon = leaves. Clay formation. Zone were parent materials weather A horizon lay Basics Start focus on A horizon Zone were parent materials weather Original rocks and minerals break down into smaller and smaller pieces Eventually dissolve A horizon Zone were new materials

More information

SELECTIVE DISSOLUTION AND DIFFERENTIAL INFRARED SPECTROSCOPY FOR CHARACTERIZATION OF 'AMORPHOUS' CONSTITUENTS IN SOIL CLAYS

SELECTIVE DISSOLUTION AND DIFFERENTIAL INFRARED SPECTROSCOPY FOR CHARACTERIZATION OF 'AMORPHOUS' CONSTITUENTS IN SOIL CLAYS Clay Minerals (1970) 8, 241. SELECTIVE DISSOLUTION AND DIFFERENTIAL INFRARED SPECTROSCOPY FOR CHARACTERIZATION OF 'AMORPHOUS' CONSTITUENTS IN SOIL CLAYS K. WADA AND D. J. GREENLAND Faculty of Agriculture,

More information

How Does Redox Status Influence Exchangeable Potassium In Soil?

How Does Redox Status Influence Exchangeable Potassium In Soil? How Does Redox Status Influence Exchangeable Potassium In Soil? Michael L. Thompson Taslima Stephen Iowa State University 1 Why do we care about exchangeable K? K is required by all plants. A soil may

More information

SOIL COLLOIDS PROPERTIES AND ION RINDING. CRC Press. University of Bueno Aires Buenos Aires, Argentina. Taylor & Francis Croup

SOIL COLLOIDS PROPERTIES AND ION RINDING. CRC Press. University of Bueno Aires Buenos Aires, Argentina. Taylor & Francis Croup SOIL COLLOIDS PROPERTIES AND ION RINDING Fernando V. Molina University of Bueno Aires Buenos Aires, Argentina CRC Press Taylor & Francis Croup Boca Raton London New York CRC Press is an imprint of the

More information

12. Lead, Pb (atomic no. 82)

12. Lead, Pb (atomic no. 82) 12. Lead, Pb (atomic no. 82) - Sources of Pb contamination include mining, metal processing, lead battery manufacturing, chemical and paint manufacturing, and lead wastes. -USEPA drinking water action

More information

Effect of Heat Treatment on Phosphate Sorption by Soils from Different Ecologies

Effect of Heat Treatment on Phosphate Sorption by Soils from Different Ecologies Effect of Heat Treatment on Phosphate Sorption by Soils from Different Ecologies 1* Aghedo, J.E., 2 Ukpebor, E. and 3 Oviasogie, P.O., 4 Omorogbe, S.O. 1Department of Chemistry, College of Education, Ekiadolor,

More information

Soil horizons differ in color, texture, structure, consistence, porosity and soil reaction.

Soil horizons differ in color, texture, structure, consistence, porosity and soil reaction. SECTION CONTENTS: The Soil Defined The Soil Profile Descriptions Of The Three Major Horizons A Fertile Soil Soil Texture Soil Structure Soil Color Soil Organisms Organic Matter Clay and Humus The Seat

More information

Phosphorus retention capacity is an important property controlling the release

Phosphorus retention capacity is an important property controlling the release Soil Chemistry Path Analysis of Phosphorus Retention Capacity in Allophanic and Non-allophanic Andisols Yohey Hashimoto* Dep. of Bioresource Science Mie Univ. Mie 514-8507, Japan Jihoon Kang Dep. of Soil

More information

Adsorption Mechanisms of Cadmium onto Pillared Clays and Chalcogenides

Adsorption Mechanisms of Cadmium onto Pillared Clays and Chalcogenides Journal of Sciences, Islamic Republic of Iran 23(3): 231-236 (2012) University of Tehran, ISSN 1016-1104 http://jsciences.ut.ac.ir Adsorption Mechanisms of Cadmium onto Pillared Clays and Chalcogenides

More information

CHARACTERIZATION OF MICROPORES OF IMOGOLITE BY MEASURING RETENTION OF QUATERNARY AMMONIUM CHLORIDES AND WATER

CHARACTERIZATION OF MICROPORES OF IMOGOLITE BY MEASURING RETENTION OF QUATERNARY AMMONIUM CHLORIDES AND WATER Clay Science 4, 127-136 (1972) CHARACTERIZATION OF MICROPORES OF IMOGOLITE BY MEASURING RETENTION OF QUATERNARY AMMONIUM CHLORIDES AND WATER K. WADA AND T. HENMI Faculty of Agriculture, Kyushu University,

More information

Volume Composition of a Desirable Surface Soil

Volume Composition of a Desirable Surface Soil Soil Chemistry Volume Composition of a Desirable Surface Soil 50% pore space 25% air 45 to 48% mineral matter 50% solid material 25% water 2 to 5% organic matter Soil Organic Matter Soil organic matter:

More information

PREPARATION OF SYNTHETIC ZEOLITES FROM COAL FLY ASH. Shamsul Kamal Sulaiman

PREPARATION OF SYNTHETIC ZEOLITES FROM COAL FLY ASH. Shamsul Kamal Sulaiman Solid State Science and Technology, Vol. 16, No 1 (28) 17-113 ISSN 128-7389 PREPARATION OF SYNTHETIC ZEOLITES FROM COAL FLY ASH Shamsul Kamal Sulaiman Mineral Research Centre, Minerals and Geoscience Department,

More information

Engineering Geology ECIV 3302

Engineering Geology ECIV 3302 Engineering Geology ECIV 3302 Instructor : Dr. Jehad Hamad 2019-2018 Chapter (5) Weathering & Soil Chapter 5: Weathering, Soil, and Mass Wasting External processes include : (1) Weathering (2) Mass wasting

More information

STUDIES ON THE SORPTION OF PHOSPHATE ON SOME SOILS OF INDIA SATURATED WITH DIFFERENT CATIONS

STUDIES ON THE SORPTION OF PHOSPHATE ON SOME SOILS OF INDIA SATURATED WITH DIFFERENT CATIONS I.J.S.N., VOL. 2(2) 211: 327-333 ISSN 2229 6441 STUDIES ON THE SORPTION OF PHOSPHATE ON SOME SOILS OF INDIA SATURATED WITH DIFFERENT CATIONS Bansal, O. P. Chemistry Department, D.S. College, Aligarh-221

More information

The Role of Soil Organic Matter in Potassium Fixation Nathan Smith

The Role of Soil Organic Matter in Potassium Fixation Nathan Smith The Role of Soil Organic Matter in Potassium Fixation Nathan Smith Undergraduate Research Assistant in Agronomy Senior in Agronomy and Environmental Science Iowa State University Soil Potassium (K + )

More information

ANION INFLUENCE ON SOME SOIL

ANION INFLUENCE ON SOME SOIL ANION INFLUENCE ON SOME SOIL PHYSICAL PROPERTIES by R. D. KREBS, G. W. THOMAS, AND J. E. MOORE Virginia Polytechnic Institute, Blacksburg, Virginia ABSTRACT Addition of HCI, H2S04, and HsPO 4 to montmorillonite

More information

Clay mineralogy and surface charge characteristics of basaltic soils from Western Samoa

Clay mineralogy and surface charge characteristics of basaltic soils from Western Samoa Clay Minerals (1997) 32, 545-556 Clay mineralogy and surface charge characteristics of basaltic soils from Western Samoa R. NADU ~, R. J. MORRSON*, L. JANK t AND M. ASGHAR ) School of Pure and Applied

More information

J. ISSAAS Vol. 20, No. 2:43-50 (2014)

J. ISSAAS Vol. 20, No. 2:43-50 (2014) J. ISSAAS Vol. 20, No. 2:43-50 (2014) EFFECTS OF SILICATE APPLICATION ON THE RELEASE PATTERN OF NATIVE INORGANIC PHOSPHORUS FROM ANDISOL SOIL IN LEMBANG, INDONESIA USING SUCCESSIVE RESIN EXTRACTION Arief

More information

ABSTRACT INTRODUCTION. Scientific registration n : 239 Symposium n : 22 Presentation : poster

ABSTRACT INTRODUCTION. Scientific registration n : 239 Symposium n : 22 Presentation : poster Scientific registration n : 239 Symposium n : 22 Presentation : poster Mineralogy and chemical properties of the Andisols from West Sumatra, Indonesia Minéralogie et propriétés chimiques des Andisols de

More information

CHAPTER 5 REVIEW. C. CO 2 D. Fe 2 O 3. A. Fe B. CO

CHAPTER 5 REVIEW. C. CO 2 D. Fe 2 O 3. A. Fe B. CO CHAPTER 5 REVIEW 1. The following represents the process used to produce iron from iron III oxide: Fe 2 O 3 + 3CO 2Fe + 3CO 2 What is the reducing agent in this process? A. Fe B. CO C. CO 2 D. Fe 2 O 3

More information

CHARGE, COLLOIDAL, A.i^«) STRUCTURAL STABILITY INTERRELATIONSHIPS FOR SELECTED HAWAII SOILS

CHARGE, COLLOIDAL, A.i^«) STRUCTURAL STABILITY INTERRELATIONSHIPS FOR SELECTED HAWAII SOILS CHARGE, COLLOIDAL, A.i^«) STRUCTURAL STABILITY INTERRELATIONSHIPS FOR SELECTED HAWAII SOILS A THESIS SUBMITTED TO THE GRADUATE DIVISION OF THE UNIVERSITY OF HAWAII IN PARTIAL FULFILLMENT OF THE REQUIREMENTS

More information

Subject Index. Darcy's law 213 deformation 235 demethylation 148,155,156,157,158,159 desmetryn 70,71

Subject Index. Darcy's law 213 deformation 235 demethylation 148,155,156,157,158,159 desmetryn 70,71 acid mine drainage 149 acidic polysaccharides 58 acidification 148,149,166 acidity 62 absorption 4, 5 adsorption 4,5,38,62, 63, 65, 66, 68, 70,71,73,77, 102, 104 free energy of 78 energy 79 Al 95 Al oxide

More information

PHOSPHORUS SORPTION CHARACTERISTICS OF SOME REPRESENTATIVE SOILS OF SOUTH INDIA

PHOSPHORUS SORPTION CHARACTERISTICS OF SOME REPRESENTATIVE SOILS OF SOUTH INDIA SAARC J. Agri., 13(1):14-26 (2015) PHOSPHORUS SORPTION CHARACTERISTICS OF SOME REPRESENTATIVE SOILS OF SOUTH INDIA I. Rashmi *, A.K. Biswas, V.R.R. Parama 1 and A.S. Rao Indian Institute of Soil Science,

More information

MINERAL CONTENT AND DISTRIBUTION AS INDEXES OF WEATHERING IN THE OMEGA AND AHMEEK SOILS OF NORTHERN WISCONSIN

MINERAL CONTENT AND DISTRIBUTION AS INDEXES OF WEATHERING IN THE OMEGA AND AHMEEK SOILS OF NORTHERN WISCONSIN MINERAL CONTENT AND DISTRIBUTION AS INDEXES OF WEATHERING IN THE OMEGA AND AHMEEK SOILS OF NORTHERN WISCONSIN By L. D. WHITTIG 1 AND M. L. JACKSON University of Wisconsin, Madison, Wisconsin ABSTRACT Quantitative

More information

Copper, Lead, Cadmium, and Zinc Sorption By Waterlogged and Air-Dry Soil

Copper, Lead, Cadmium, and Zinc Sorption By Waterlogged and Air-Dry Soil I. R. Phillips Journal of Soil Contamination, 8(3):343 364 (1999) Copper, Lead, Cadmium, and Zinc Sorption By Waterlogged and Air-Dry Soil School of Environmental Engineering, Griffith University, Nathan,

More information

Weathering and Soils

Weathering and Soils OCN 401-17 Aug. 29, 2016 KCR Weathering and Soils Biogeochemistry Chapter 4: The Lithosphere Introduction: the context Rock Weathering Soil Chemical Reactions Soil Development (see text) Weathering Rates

More information

Soil Biogeochemistry. Introduction. Soil Formation and Pedogenesis

Soil Biogeochemistry. Introduction. Soil Formation and Pedogenesis Soil Biogeochemistry 2 Introduction If you consider all the ways in which soils influence element cycling, hydrologic cycling, species diversity, biotic growth, productivity, and global carbon storage,

More information

HUMUS CHEMISTRY. Genesis, Composition, Reactions. Second Edition. F. J. STEVENSON Department of Agronomy University of Illinois

HUMUS CHEMISTRY. Genesis, Composition, Reactions. Second Edition. F. J. STEVENSON Department of Agronomy University of Illinois JOHN WILEY & SONS, INC. HUMUS CHEMISTRY Genesis, Composition, Reactions Second Edition F. J. STEVENSON Department of Agronomy University of Illinois New York Chichester Brisbane Toronto Singapore CONTENTS

More information

Supplemental Materials. Sorption of Tetracycline to Varying-Sized Montmorillonite Fractions

Supplemental Materials. Sorption of Tetracycline to Varying-Sized Montmorillonite Fractions Supplemental Materials Sorption of Tetracycline to Varying-Sized Montmorillonite Fractions 6 7 8 9 10 11 1 Huaizhou Xu, 1, Xiaolei Qu, 1 Hui Li, Cheng Gu 1, and Dongqiang Zhu 1* 1 State Key Laboratory

More information

From soil clays to erosion processes Jaime Cuevas UAM

From soil clays to erosion processes Jaime Cuevas UAM From soil clays to erosion processes Jaime Cuevas UAM Clay erosion in safety assessment in Deep Geological Repositories (DGR) Compacted bentonite will produce colloidal particles (Fissures; active fractures)

More information

Only healthy soil can grow a nutrient dense food. You are what you eat!

Only healthy soil can grow a nutrient dense food. You are what you eat! Understanding How Cation Nutrients & Soil Structure are Related By Michael Martin Meléndrez Only healthy soil can grow a nutrient dense food. You are what you eat! Soil Must be able to hold onto water,

More information

Weathering and Soils

Weathering and Soils OCN 401-11 Oct. 13, 2011 KCR Weathering and Soils Biogeochemistry Chapter 4: The Lithosphere Introduction: the context Rock Weathering Soil Chemical Reactions Soil Development (see text) Weathering Rates

More information

Circle the correct (best) terms inside the brackets:

Circle the correct (best) terms inside the brackets: 1 Circle the correct (best) terms inside the brackets: 1) Soils are [consolidated / unconsolidated] [natural / artificial] bodies at the earth s surface. Soils contain mineral and organic material, which

More information

A thesis submitted to the University of Manchester for the degree of Doctor of Philosophy in the Faculty of Engineering and Physical Sciences

A thesis submitted to the University of Manchester for the degree of Doctor of Philosophy in the Faculty of Engineering and Physical Sciences Organic ligand complexation reactions on aluminium-bearing mineral surfaces studied via in-situ Multiple Internal Reflection Infrared Spectroscopy, adsorption experiments, and surface complexation modelling

More information

Lecture 29: Soil Formation

Lecture 29: Soil Formation Lecture 29: Soil Formation Factors Controlling Soil Formation 1. Parent material: Soil precursor 2. Climate: Temperature and precipitation 3. Biota: Native vegetation, microbes, soil animals, humans 4.

More information

Soil physical and chemical properties the analogy lecture. Beth Guertal Auburn University, AL

Soil physical and chemical properties the analogy lecture. Beth Guertal Auburn University, AL Soil physical and chemical properties the analogy lecture. Beth Guertal Auburn University, AL Soil Physical Properties Porosity Pore size and pore size distribution Water holding capacity Bulk density

More information

Technical Data Sheet Tersil COR

Technical Data Sheet Tersil COR Technical Data Sheet Tersil COR 1. CLAY MINERAL ACTIVE INGREDIENTS Clay mineral is a natural raw material of mineral origin, composed of extremely fine particles of silicates, as well as several microminerals.

More information

BASELINE STUDIES OF THE CLAY MINERALS SOCIETY SOURCE CLAYS: CHEMICAL ANALYSES OF MAJOR ELEMENTS

BASELINE STUDIES OF THE CLAY MINERALS SOCIETY SOURCE CLAYS: CHEMICAL ANALYSES OF MAJOR ELEMENTS Clays and Clay Minerals, Vol. 49, No. 5, 381 386, 2001. BALINE STUDIES OF THE CLAY MINERALS SOCIETY SOURCE CLAYS: CHEMICAL ANALYS OF MAJOR ELEMENTS AHMET R. MERMUT 1 AND ANGEL FAZ CANO 2 1 University of

More information

THE PHOSPHORUS SORPTION POTENTIAL OF SELECTED HAWAIIAN SOILS IN RELATION TO THEIR MINERALOGY AND CHEMISTRY

THE PHOSPHORUS SORPTION POTENTIAL OF SELECTED HAWAIIAN SOILS IN RELATION TO THEIR MINERALOGY AND CHEMISTRY THE PHOSPHORUS SORPTION POTENTIAL OF SELECTED HAWAIIAN SOILS IN RELATION TO THEIR MINERALOGY AND CHEMISTRY A THESIS SUBMITTED TO THE GRADUATE DIVISION OF THE UNIVERSITY OF HAWAII IN PARTIAL FULFILLMENT

More information

Adsorption Isotherm of Phosphate Ions onto lica and Amino-modified lica from Lapindo Mud Jaslin Ikhsan 1,2, ti Sulastri 1, Erfan Priyambodo 1 1 Department of Chemistry Education, Faculty of Mathematics

More information

MODELING OF SOIL CATION EXCHANGE CAPACITY BASED ON SOME SOIL PHYSICAL AND CHEMICAL PROPERTIES

MODELING OF SOIL CATION EXCHANGE CAPACITY BASED ON SOME SOIL PHYSICAL AND CHEMICAL PROPERTIES MODELING OF SOIL CATION EXCHANGE CAPACITY BASED ON SOME SOIL PHYSICAL AND CHEMICAL PROPERTIES Majid Rashidi 1 and Mohsen Seilsepour 2 1 Department of Agricultural Machinery, Faculty of Agriculture, Islamic

More information

Earth: An Introduction to Physical Geology Weathering and Soil

Earth: An Introduction to Physical Geology Weathering and Soil Chapter 6 Lecture Earth: An Introduction to Physical Geology Eleventh Edition Weathering and Soil Tarbuck and Lutgens Weathering Weathering involves the physical breakdown and chemical alteration of rock

More information

Shirley E. Clark, Ph.D., P.E., D. WRE Penn State Harrisburg. Robert Pitt, Ph.D., P.E., BCEE, D. WRE University of Alabama

Shirley E. Clark, Ph.D., P.E., D. WRE Penn State Harrisburg. Robert Pitt, Ph.D., P.E., BCEE, D. WRE University of Alabama Shirley E. Clark, Ph.D., P.E., D. WRE Penn State Harrisburg Robert Pitt, Ph.D., P.E., BCEE, D. WRE University of Alabama Site Stormwater Characteristics and Permit Limits Analytes on Permit 90 th percentile

More information