Be sure to show all calculations so that you can receive partial credit for your work!

Size: px
Start display at page:

Download "Be sure to show all calculations so that you can receive partial credit for your work!"

Transcription

1 Agronomy 365T Exam 1 Spring 2004 Exam Score: Name TA Lab Hour Be sure to show all calculations so that you can receive partial credit for your work! 1) List 14 of the plant essential nutrient for plant growth (excluding C, H, O). Provide the complete name of the element, one form taken up by plants and list if the nutrient is a macro- or micronutrient. Spelling and charge count! (7 points) Essential Nutrient Form taken up by plant Macro or Micro including valence ) List the three nutrients categorized as secondary: (3 points) 3) What nutrient deficiencies are shown in the pictures projected. (3 points) a) b) c)

2 2 4) Define or explain the following terms as they relate to Soil Fertility: (2 points each, 6 points total) Liebig s Law of the Minimum ph (and indicate the normal range found for soils in the Midwest) Apoplastic Transport 5) What two factors control the differences in cation retention in soils (the lyotropic series: why ions are held in this order Al > Ca > Mg > K > Na)? (2 points each, 4 points) ) Your sand greens (1% O.M) on your golf course have CEC values of only 2 meq/100g. You want to increase the CEC to enhance nutrient retention. (4 points) a) Would it be better to increase the CEC of the soil by lowering or raising the soil ph to increase the CEC? b) What other practice might you use to raise the CEC of this soil? 7) The primary function in the plant of each of these nutrients is (4 points) Nutrient Magnesium Phosphorus Primary Function in the Plant

3 8) CEC Calculations - Use the following data for problems a through f: (6 points) 3 Soil Test Report ph OM P K Mg Ca H Al CEC % B.S. (%) (ppm) meq/100g (meq/100g) (%)? ?? a) Calculate the CEC of this soil. b) Calculate the % Base Saturation of this soil. c) Calculate the pounds per acre of magnesium in this soil. (Hint : AFS = 2,000,000 lbs. and the atomic weight of Mg= 24g) d) What is the estimated ph of this soil? e) Should you use dolomitic or calcitic lime to raise the ph of this soil? f) Calculate the pounds per acre of phosphorus in this soil. 9) If a soil has a CEC of 30 cmol(+)/kg and a base saturation of 40% (ph 5), how much CaCO 3 (Molec. Wt. = 100g) would it take to raise this soil to a ph of 7? (2 points) 10) Clay Minerals - Match one of the clay minerals in the right column to the property listed in the left column. (5 points) Commonly found in Vertisols 1:1 clay mineral Contains interlayer potassium CEC of approximately 100 meq/100g Has significant isomorphous substitution of Mg for Al in the octahedral sheet A. Montmorillonite B. Illite C. Kaolinite

4 4 11) Discuss the relationship of cation exchange capacity to buffering capacity to lime requirement of soils. (5 points) 12) A golf course superintendent calls you and says that the grass in one of his fairways keeps dying even though he gives it plenty of water and fertilizer and that compaction is not a problem. You ask him the soil ph and he says, Why do you care about soil ph? You give him the following 4 (four) reasons why soil ph is so important. (4 points) ) We know that the molecular weight of MgCO 3 = 84 g mole -1, and that the equivalent weight of MgCO 3 = 42g mole -1. We also know that the molecular weight of CaCO 3 is 100 g mole -1 and that the equivalent weight of CaCO 3 is 50 g mole -1. Show all work!!! What is the calcium carbonate equivalent (CCE) of MgCO 3? (3 points) 14) If the sieve analysis of the MgCO 3 from Question 13 showed that 80 percent of this material passed an 8-mesh sieve and 40 percent of it passed a 60-mesh sieve: a) What is the Fineness Factor for this material in the U.S.A.? (3 points) b) What is the Relative Neutralizing Value (RNV) or the Effective Calcium Carbonate Equivalent (ECCE) of this material? (2 points) [If you could not calculate the answer to Ques. 13, assume the CCE of MgCO 3 is 110%]

5 5 15) Based on the following information: Wheat crop transpired 2.8 million lbs of water Root volume was 1.0 % of soil volume all the way to 12 inches Wheat crop accumulates 30 lb P/acre Nutrient concentrations in soil solution and total available nutrients in top 12 inches. Total available Nutrient Soil solution concentration in top 12 inches mg L -1 lb/acre P Please calculate how many lbs P acre -1 would be delivered to the wheat crop via the following mechanisms: Show all work!!! Root Interception: (2 points) Mass Flow: (2 points) Diffusion: (2 points) 16) For the three soils on display, answer the following questions. a) Estimate the C.E.C. of the upper 7 inches of Soil A, Soil B and Soil C. (6 pts.) - SHOW CALCULATIONS AND ASSUMPTIONS - Soil A (silt loam soil, 20% clay- Indiana) meq/100 g Soil B (silty clay loam, 30% clay - Indiana) meq/100 g Soil C (tropical Oxisol, 50% clay/hydrous oxides-brazil) meq/100 g b) Which soil contains the most hematite? c) Which soil contains the most montmorillonite? d). Which soil is most likely to have an anion exchange capacity at ph 4?

6 6 Multiple Choice Select the best answer to each question and record your answer in the blank to the left of the question number. (2 pts each) 1. Phosphorus and potassium move to root surfaces predominately by: A. root interception B. mass flow C. diffusion 2. The availability of Fe, Mn, Zn, and Cu increases as soil ph A. increases B. decreases C. exceeds A soil containing 10% kaolinite, 10 % montmorillonite, and 10% illite and 4% organic matter would probably have a CEC of approximately A. 6 meq/100 g B. 12 meq/100 g C. 23 meq/100 g D. 36 meq/100 g 4. Under what conditions would a soil most likely have a significant anion exchange capacity A. a midwestern soil having a ph of 6.8 and containing predominantly illite clay B. a highly weathered soil containing kaolinite and hydrous oxides of iron and alluminum at ph 4.3 C. a midwestern soil with predominantly montmorillinite clay and a ph of 6.2 D. an alluvial soil along the Amazon River with predominately montmorillonite and kaolinite and having a ph of The typical cation distribution on the exchange sites of a fertile Indiana soil with a ph 6.5 would have the relative milliequivalents of A. acidic cations greater than basic cations with Ca and Mg being in greater amounts than K and Na B. acidic cations less than basic cations with Ca and Mg being in lesser amounts than K and Na C. acidic cations less than basic cations with Ca and Mg being in greater amounts than K and Na D. acidic cations greater than basic cations with Ca and Mg in lesser amounts than K and Na

7 7 6. A soil with a hydrogen ion concentration of 4.0 X 10-5 N would have a ph of A. 4.0 log 3 = 0.48 B. 5.0 log 4 = 0.60 C. 5.4 log 5 = 0.70 D. 4.4 E A soil with a ph of 4.7 would have most of its acidity as A. active acidity. B. reserve acidity. 8. If an acre of soil requires 9,000 pounds of pure calcium carbonate to raise its ph from 5 to 6, approximately how many pounds of sulfur would it require to lower the ph from 6 to 5 (Formula weight: CaCO 3 = 100 g, S = 32 g). A lb B lb C lb D lb E. 15,600 lb 9. An acid soil (ph 4.5) with a large amount of ph dependent charge can not accurately have its lime recommendations determined using the SMP Buffer (ph 7.5). Does the Buffer Method over-estimate or under-estimate lime requirement. A. over estimates B. under estimates 10. The parent material (C horizon) of a glacial till derived soil in Indiana contains mostly calcareous till (Ca saturated exchange sites and free CaCO 3 ), what is the ph of this material. A. 9.2 B. 8.2 C. 7.2 D. 6.2 E. 5.2

8 8 Questions 11 and 12 - Answer these two questions based on the data given Soil A Soil B Soil-water ph SMP Buffer ph Which of these Indiana soils requires more lime to raise soil ph to 6.5? A. Soil A B. Soil B C. The same, (ph = 5.2) 12. Which Indiana soil has the greater cation exchange capacity (C.E.C)? A. Soil A B. Soil B C. CEC is the same 13. Most of the cation exchange capacity on organic matter originates from: A. isomorphous substitution and it is ph dependent. B. dissociation of H from carboxylic acid groups and it is ph dependent. C. isomorphic substitution and it is not ph dependent. D. dissociation of H from carboxylic acid groups and it is not ph dependent. E. dissociation of SiOH groups on the edge of the crystal structure of the O.M and it is ph dependent. 14. Which of these materials is a good soil acidifying material, is very insoluble in water, and requires microbial activity to release acidity into the soil? A. Sulfur B. Ammonium sulfate C. Gypsum CaSO 4 D. Iron Sulfate E. CaCl 2

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

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

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

ph and Liming Practices Kent Martin Stafford County 1/5/2010

ph and Liming Practices Kent Martin Stafford County 1/5/2010 ph and Liming Practices Kent Martin Stafford County 1/5/2010 Outline What is ph Normal ph ranges Acid Soil Importance of soil ph Factors affecting soil ph Acid types and measurement Neutralizing value

More information

Agricultural Fertilizer Applicator Soil Test Results What the heck do they mean?

Agricultural Fertilizer Applicator Soil Test Results What the heck do they mean? Agricultural Fertilizer Applicator Soil Test Results What the heck do they mean? Northeast Ohio Pesticide Safety Education Program Lee Beers, OSU Extension Trumbull County beers.66@osu.edu 330-638-6783

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

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

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

Gain a better understanding of soil ph and how it is measured. Understand how lime requirement is determined.

Gain a better understanding of soil ph and how it is measured. Understand how lime requirement is determined. LABORATORY 7 SOIL REACTION (ph) AND LIME REQUIREMENT I Objectives Gain a better understanding of soil ph and how it is measured. Understand how lime requirement is determined. II Introduction A Soil Reaction

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

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

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

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

FOR Soil Quality Report 2017

FOR Soil Quality Report 2017 Student Name: Partner Name: Laboratory Date: FOR 2505 - Soil Quality Report 2017 Objectives of this report: 10 Marks Lab Objectives Section Principles behind methods used to determine soil base cation

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

Grower: Obion Grain Farm: Multi-Farm Acres: Field(s): Multi-Field

Grower: Obion Grain Farm: Multi-Farm Acres: Field(s): Multi-Field Data Manager Farm: Multi-Farm Acres: 205.23 Field(s): Multi-Field Farm-Field Map *NOTE: The field labels above are actual FIELD NAMES. N ISSUED: 2:50pm EDT Oct 9, 2009 Data Manager Farm-Field Reference

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

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 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

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

Running head: TITLE 1. Lab Report. Name. Academic Institution. Author Note. Class. Professor

Running head: TITLE 1. Lab Report. Name. Academic Institution. Author Note. Class. Professor Running head: TITLE 1 Lab Report Name Academic Institution Author Note Class Professor March 13, 2018 TITLE 2 Soil colloids tend to have a net negative charge for two reasons: surface area and ph levels.

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

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

Soils. Source: Schroeder and Blum, 1992

Soils. Source: Schroeder and Blum, 1992 Soils Source: Schroeder and Blum, 1992 Literature cited: Schroeder, D. and Blum, W.E.H. 1992. Bodenkunde in Stichworten. Gebrüder Borntraeger, D-1000 Berlin. Geology and Life Conceptual model Source: Knight,

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

Lab 8 Dynamic Soil Systems I: Soil ph and Liming

Lab 8 Dynamic Soil Systems I: Soil ph and Liming Lab 8 Dynamic Soil Systems I: Soil ph and Liming Objectives: To measure soil ph and observe conditions which change ph To distinguish between active acidity (soil solution ph) and exchangeable acidity

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

Understanding and Interpreting Soil and Plant Tissue Lab Reports

Understanding and Interpreting Soil and Plant Tissue Lab Reports Understanding and Interpreting Soil and Plant Tissue Lab Reports Dirk Holstege Director, UC Davis Analytical Laboratory dmholstege@ucdavis.edu 530-752-0148 224 Hoagland Hall UC Davis Anlab.ucdavis.edu

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

MODULE 5.2 Soil properties

MODULE 5.2 Soil properties MODULE 5.2 Soil properties Exchangeable cations and cation exchange capacity 3 Acid - Base Ion Exchange Reaction In Soils 3 Anion retention 5 Soil Profile And Its Importance 7 Water, air and particles

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

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

WEATHERING ACCORDING TO THE CATIONIC BONDING ENERGIES OF COLLOIDS I ABSTRACT

WEATHERING ACCORDING TO THE CATIONIC BONDING ENERGIES OF COLLOIDS I ABSTRACT WEATHERING ACCORDING TO THE CATIONIC BONDING ENERGIES OF COLLOIDS I By E. R. GRAHAM University of Missouri ABSTRACT A study was made of the energy changes of several colloidal systems in relation to weathering.

More information

Soil - the battery of your business

Soil - the battery of your business Soil - the battery of your business By DAVID HANLON The basis of our farm business is the soil and increasingly all growers are focusing their attention on this vital resource. Just what state it is in

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

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

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

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

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

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

REVIEW OF BASIC CHEMISTRY ANSWER KEY

REVIEW OF BASIC CHEMISTRY ANSWER KEY REVIEW OF BASIC CHEMISTRY ANSWER KEY 1. Name the following elements. Spelling counts: 2. Write the symbols for the following elements. H hydrogen sodium Na S sulphur phosphorus P Cl chlorine fluorine F

More information

Sedimentary Geology. Strat and Sed, Ch. 1 1

Sedimentary Geology. Strat and Sed, Ch. 1 1 Sedimentary Geology Strat and Sed, Ch. 1 1 Sedimentology vs. Stratigraphy Sedimentology is the study of the origin and classification of sediments and sedimentary rocks Mostly the physical and chemical

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

Processed Food Production. Consistent product Long shelf life Low cost

Processed Food Production. Consistent product Long shelf life Low cost How is the production of wheat connected to Earth and environmental sciences? Processed Food Production Consistent product Long shelf life Low cost Twinkie Ingredients Enriched bleached wheat flour [flour,

More information

CHEMISTRY 102B Practice Hour Exam I. Dr. D. DeCoste T.A (30 pts.) 16 (15 pts.) 17 (15 pts.) Total (60 pts)

CHEMISTRY 102B Practice Hour Exam I. Dr. D. DeCoste T.A (30 pts.) 16 (15 pts.) 17 (15 pts.) Total (60 pts) CHEMISTRY 102B Practice Hour Exam I Spring 2016 Dr. D. DeCoste Name Signature T.A. This exam contains 17 questions on 5 numbered pages. Check now to make sure you have a complete exam. You have one hour

More information

HANDOUT SET GENERAL CHEMISTRY I

HANDOUT SET GENERAL CHEMISTRY I HANDOUT SET GENERAL CHEMISTRY I Periodic Table of the Elements 1 2 3 4 5 6 7 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 IA VIIIA 1 2 H He 1.00794 IIA IIIA IVA VA VIA VIIA 4.00262 3 Li 6.941 11 Na 22.9898

More information

Chapter 6. Weathering, Erosion, and Soil

Chapter 6. Weathering, Erosion, and Soil Chapter 6 Weathering, Erosion, and Soil Introduction Rocks and minerals disintegrate and decompose by the processes of physical and chemical weathering. This breakdown occurs because the parent material

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

Soil Chemical Composition and Fertility Management Mary-Howell R. Martens. Originally Printed in Acres USA, 2001

Soil Chemical Composition and Fertility Management Mary-Howell R. Martens. Originally Printed in Acres USA, 2001 Soil Chemical Composition and Fertility Management Mary-Howell R. Martens Originally Printed in Acres USA, 2001 Wise soil management - throughout history, it has been the foundation of all great civilizations

More information

Mehlich and Modified Mehlich Buffer for Lime Requirement

Mehlich and Modified Mehlich Buffer for Lime Requirement Mehlich and Modified Mehlich Buffer for Lime Requirement David H. Hardy Application and Principle The development of the Mehlich buffer was to estimate acidity actually affecting plant growth in North

More information

Tikrit University. College of Engineering Civil engineering Department SOIL PROPERTES. Soil Mechanics. 3 rd Class Lecture notes Up Copyrights 2016

Tikrit University. College of Engineering Civil engineering Department SOIL PROPERTES. Soil Mechanics. 3 rd Class Lecture notes Up Copyrights 2016 Tikrit University SOIL PROPERTES College of Engineering Civil engineering Department Soil Mechanics 3 rd Class Lecture notes Up Copyrights 2016 1-Soil Composition -Solids -Water -Air 2-Soil Phases -Dry

More information

Aquatic Chemistry (10 hrs)

Aquatic Chemistry (10 hrs) Aquatic Chemistry (10 hrs) Water -The quality and quantity of water available to human have been vital factors in determining their well-being. -More then 70% of the earth is covered by water. Living cells

More information

1) What is the volume of a tank that can hold Kg of methanol whose density is 0.788g/cm 3?

1) What is the volume of a tank that can hold Kg of methanol whose density is 0.788g/cm 3? 1) Convert the following 1) 125 g to Kg 6) 26.9 dm 3 to cm 3 11) 1.8µL to cm 3 16) 4.8 lb to Kg 21) 23 F to K 2) 21.3 Km to cm 7) 18.2 ml to cm 3 12) 2.45 L to µm 3 17) 1.2 m to inches 22) 180 ºC to K

More information

Effect of integrated nutrient management practices on acidity and nutrient availability in acid soil

Effect of integrated nutrient management practices on acidity and nutrient availability in acid soil 207; 5(4): 678-682 P-ISSN: 2349 8528 E-ISSN: 232 4902 IJCS 207; 5(4): 678-682 207 JEZS Received: 03-05-207 Accepted: 04-06-207 Tupaki Lokya Agriculture Chemistry, OUAT, J Ravinder Agriculture Chemistry,

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

Lect. 2: Chemical Water Quality

Lect. 2: Chemical Water Quality The Islamic University of Gaza Faculty of Engineering Civil Engineering Department M.Sc. Water Resources Water Quality Management (ENGC 6304) Lect. 2: Chemical Water Quality ١ Chemical water quality parameters

More information

Sedimentary Rocks and Processes

Sedimentary Rocks and Processes Sedimentary Rocks and Processes Weathering Sedimentary Processes Breakdown of pre-existing rock by physical and chemical processes Transport Movement of sediments from environments of relatively high potential

More information

CHEM 60 Spring 2016 Exam 2 Ch 5-8, 100 points total.

CHEM 60 Spring 2016 Exam 2 Ch 5-8, 100 points total. Name Exam No. F CHEM 60 Spring 2016 Exam 2 Ch 5-8, 100 points total. Multiple Choice. (20 questions, 3 points each = 60 points total) Mark the letter on the scantron form corresponding to the one best

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 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

Alleviating Soil Acidity through Organic Matter Management. Malcolm E. Sumner, University of Georgia Marcos A Pavan IAPAR

Alleviating Soil Acidity through Organic Matter Management. Malcolm E. Sumner, University of Georgia Marcos A Pavan IAPAR Alleviating Soil Acidity through Organic Matter Management Malcolm E. Sumner, University of Georgia Marcos A Pavan IAPAR Introduction Most work on topsoil acidity amelioration Mechanical lime incorporation

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

Ch. 4 - Clay Minerals, Rock Classification Page 1. Learning Objectives. Wednesday, January 26, 2011

Ch. 4 - Clay Minerals, Rock Classification Page 1. Learning Objectives. Wednesday, January 26, 2011 Ch. 4 - Clay Minerals, Rock Classification Page 1 Learning Objectives Ch. 4 - Clay Minerals, Rock Classification Page 2 Symbols Ch. 4 - Clay Minerals, Rock Classification Page 3 Clay Minerals and Structure

More information

Chapter 6 9/25/2012. Weathering, Erosion and Soils. Introduction. How Are Earth Materials Altered? Introduction. How Are Earth Materials Altered?

Chapter 6 9/25/2012. Weathering, Erosion and Soils. Introduction. How Are Earth Materials Altered? Introduction. How Are Earth Materials Altered? Chapter 6 Introduction Rocks and minerals are disintegrated and decomposed by the processes of mechanical and chemical weathering. Weathering, Erosion and Soils This breakdown occurs because the parent

More information

HETEROGENEITY IN MONTMORILLONITE. JAMES L. MCATEE, JR. Baroid Division, National Lead Co., Houston, Texas

HETEROGENEITY IN MONTMORILLONITE. JAMES L. MCATEE, JR. Baroid Division, National Lead Co., Houston, Texas HETEROGENEITY IN MONTMORILLONITE By JAMES L. MCATEE, JR. Baroid Division, National Lead Co., Houston, Texas ABSTRACT X-ray diffraction patterns and cation-exchange data are presented for centrifuged Wyoming

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

Chem 101 Practice Exam 3 Fall 2012 You will have a Solubility Table and Periodic Table

Chem 101 Practice Exam 3 Fall 2012 You will have a Solubility Table and Periodic Table Chem 101 Practice Exam Fall 01 You will have a Solubility Table and Periodic Table 1. A 1.6-mol sample of KClO was decomposed according to the equation KClO (s) KCl(s) O (g) How many moles of O are formed

More information

Atoms, the basic building block of matter, are composed of three basic particles. Nucleus: Proton (+) Neutron (-) Outside the nucleus: Electron (-)

Atoms, the basic building block of matter, are composed of three basic particles. Nucleus: Proton (+) Neutron (-) Outside the nucleus: Electron (-) Atoms, the basic building block of matter, are composed of three basic particles Nucleus: Proton (+) Neutron (-) Outside the nucleus: Electron (-) Atomic number = # protons Atomic mass number = # protons

More information

Name: Period: Score: Everything About Chemical Formulas

Name: Period: Score: Everything About Chemical Formulas Name: Period: Score: Everything About Formulas Compounds have unique names that identify them for us when we study chemical properties and changes. Chemists have devised a shorthand way of representing

More information

Plant Nutrition and Transport. Chapter 29

Plant Nutrition and Transport. Chapter 29 Plant Nutrition and Transport Chapter 29 Overview: Underground Plants The success of plants depends on their ability to gather and conserve resources from their environment. The transport of materials

More information

ENVI.2030L - Minerals

ENVI.2030L - Minerals ENVI.2030L - Minerals Name I. Minerals Minerals are crystalline solids - the particles (atoms) that make-up the solid have a regular arrangement. In glasses, on the other hand, the atoms are not arranged

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

Use of Western Pozzolan ATS soil amendment for golf course fairways.

Use of Western Pozzolan ATS soil amendment for golf course fairways. Use of Western Pozzolan ATS soil amendment for golf course fairways. Study was undertaken to examine the properties of Western Pozzolan material for use in golf course fairways to improve water relations

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

Section EXAM III Total Points = 150. November 15, Each student is responsible for following directions. Read this page carefully.

Section EXAM III Total Points = 150. November 15, Each student is responsible for following directions. Read this page carefully. Name Chemistry 11100 Test 66 Section EXAM III Total Points = 150 TA Thursday, 8:00 PM November 15, 2012 Directions: 1. Each student is responsible for following directions. Read this page carefully. 2.

More information

Lecture 2: Soil Properties and Groundwater Flow

Lecture 2: Soil Properties and Groundwater Flow ENGI 7718 Environmental Geotechniques ENGI 9621 Soil Remediation Engineering Lecture 2: Soil Properties and Groundwater Flow Spring 2011 Faculty of Engineering & Applied Science 1 2.1 Soil properties 2.1.1

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

Section EXAM II Total Points = 150. October 15, Each student is responsible for following directions. Read this page carefully.

Section EXAM II Total Points = 150. October 15, Each student is responsible for following directions. Read this page carefully. Name Chemistry 11100 Test 55 Section EXAM II Total Points = 150 TA Monday, 6:30 PM October 15, 2012 Directions: 1. Each student is responsible for following directions. Read this page carefully. 2. Write

More information

THE UNPREDICTABILITY OF SOIL FERTILITY ACROSS SPACE AND TIME

THE UNPREDICTABILITY OF SOIL FERTILITY ACROSS SPACE AND TIME THE UNPREDICTABILITY OF SOIL FERTILITY ACROSS SPACE AND TIME R. L. Hoskinson Idaho National Engineering and Environmental Laboratory Department of Energy Idaho Falls, Idaho D. Pokrajac and Z. Obradovic

More information

8. Relax and do well.

8. Relax and do well. CHEM 1215 Exam I John I. Gelder September 15, 1999 Name TA's Name Lab Section Please sign your name below to give permission to post your course scores on homework, laboratories and exams. If you do not

More information

AGRONOMIC POTENTIAL AND LIMITATIONS OF USING PRECIPITATED CALCIUM CARBONATE IN THE HIGH PLAINS

AGRONOMIC POTENTIAL AND LIMITATIONS OF USING PRECIPITATED CALCIUM CARBONATE IN THE HIGH PLAINS GRONOMIC POTENTIL ND LIMITTIONS OF USING PRECIPITTED CLCIUM CRONTE IN THE HIGH PLINS Gary W Hergert*, Murali K Darapuneni, Robert H. Wilson, Robert M. Harveson, Jeffrey D. radshaw and Rex. Nielsen University

More information

Monument Valley, Utah. What weathering processes contributed to the development of these remarkable rock formations? Weathering Mechanisms

Monument Valley, Utah. What weathering processes contributed to the development of these remarkable rock formations? Weathering Mechanisms Monument Valley, Utah. What weathering processes contributed to the development of these remarkable rock formations? Weathering Includes Physical, Chemical, Biological processes WEATHERING CHAPTER 7 Weathering

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

(Graph #1) Cation Conc. before Mitigation, after Gypsum, & after Liqua-Jip 0"-12" Sampling Before Gypsum Liqua-Jip

(Graph #1) Cation Conc. before Mitigation, after Gypsum, & after Liqua-Jip 0-12 Sampling Before Gypsum Liqua-Jip LIQUA-JIP TEST DATA On farms with good records, some blocks of land data had been taken both before and after the application of extensive quantities of gypsum. This product has no sulfate ion in the formulation

More information

Chemical Hydrogeology

Chemical Hydrogeology Physical hydrogeology: study of movement and occurrence of groundwater Chemical hydrogeology: study of chemical constituents in groundwater Chemical Hydrogeology Relevant courses General geochemistry [Donahoe]

More information

H + OH - H + OH - H +OH -

H + OH - H + OH - H +OH - Objectives SOIL CHEMISTRY Reading Materials: Brady NC, 1990. The Nature and Properties of Soils Supardi, 1989. Sifat dan Ciri Tanah Soil ph Cation exchange o Cation Exchange Capacity (CEC) o Base saturation

More information

Feedback between nutrient availability, NPP and N release

Feedback between nutrient availability, NPP and N release Feedback between nutrient availability, NPP and N release 1 Redfield ratios A typical plant = 45% C, 1.5% N, 0.2%P or C:N = 30 : 1 and C:P = 225 : 1 or C:N:P = 225 : 7.5 : 1 N:P = 7.5 : 1 Mobility of nutrients

More information

Lab Day and Time: Instructions. 1. Do not open the exam until you are told to start. Page # Points possible Points awarded

Lab Day and Time: Instructions. 1. Do not open the exam until you are told to start. Page # Points possible Points awarded Name: Lab Day and Time: Instructions 1. Do not open the exam until you are told to start. 2. This exam is closed note and closed book. You are not allowed to use any outside material while taking this

More information

C2.6 Quantitative Chemistry Foundation

C2.6 Quantitative Chemistry Foundation C2.6 Quantitative Chemistry Foundation 1. Relative masses Use the periodic table to find the relative masses of the elements below. (Hint: The top number in each element box) Hydrogen Carbon Nitrogen Oxygen

More information

Dr. Bolaños CHEM Exam #2A Fall 2014

Dr. Bolaños CHEM Exam #2A Fall 2014 Name: Date: There are 8 questions (with parts) on this examination totaling 105 points (scored out of 100 points). You have 1.5 hours to complete this examination and may only use a basic scientific calculator

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

SoilGen2 model: data requirements and model output

SoilGen2 model: data requirements and model output SoilGen2 model: data requirements and model output 1. Essential plot data... 1 2. Essential soil data... 2 3. Precipitation data (for a typical year)... 2 4. Evapotranspiration and Air temperature data

More information

Weathering: the disintegration, or breakdown of rock material

Weathering: the disintegration, or breakdown of rock material Weathering: the disintegration, or breakdown of rock material Mechanical Weathering: no change in chemical composition--just disintegration into smaller pieces Chemical Weathering: breakdown as a result

More information

POTASSIUM ADSORPTION CHARACTERISTICS OF FOUR DIFFERENT TEXTURED ALKALINE CALCAREOUS SOILS

POTASSIUM ADSORPTION CHARACTERISTICS OF FOUR DIFFERENT TEXTURED ALKALINE CALCAREOUS SOILS Pak. J. Agri. Sci., Vol. 44(2), 2007 POTASSIUM ADSORPTION CHARACTERISTICS OF FOUR DIFFERENT TEXTURED ALKALINE CALCAREOUS SOILS Abdul Hannan*, A.M. Ranjha**, Rahmatullah**, M. Waqas*** and Abid Niaz****

More information

TREATMENT OF LANDFILL LEACHATE USING ZEOLITE

TREATMENT OF LANDFILL LEACHATE USING ZEOLITE TREATMENT OF LANDFILL LEACHATE USING ZEOLITE Grant Redvers and Renate Timm (City Design Ltd), Garry Peters (Auckland City Council) and Craig Mowatt (NZ Natural Zeolite Ltd) Introduction City Design Ltd,

More information

Treatment of Salt Affected Soil in the Oil Field

Treatment of Salt Affected Soil in the Oil Field Treatment of Salt Affected Soil in the Oil Field Abstract Soils, drill cuttings and other solid wastes which are exposed to high levels of salt through spillage from drilling and producing operations,

More information

CHEMISTRY 101 Hour Exam I. Dr. D. DeCoste T.A (30 pts.) 16 (15 pts.) 17 (15 pts.) Total (60 pts)

CHEMISTRY 101 Hour Exam I. Dr. D. DeCoste T.A (30 pts.) 16 (15 pts.) 17 (15 pts.) Total (60 pts) CHEMISTRY 101 Hour Exam I February 9, 2017 Dr. D. DeCoste Name Signature T.A. This exam contains 17 questions on 6 numbered pages. Check now to make sure you have a complete exam. You have one hour and

More information

CHEMISTRY 101 EXAM 1 FORM 1J

CHEMISTRY 101 EXAM 1 FORM 1J CHEMISTRY 101 EXAM 1 SECTIONS 540-550 Dr. Joy Heising FORM 1J September 26, 2003 Directions: 1. This examination consists of two parts: 17 multiple choice questions (4 points each) in Part 1 and 3 free

More information

Department of Agricultural Chemistry and Soil Science, University College of Agriculture, Calcutta University, Calcutta 700 0\ 9, India

Department of Agricultural Chemistry and Soil Science, University College of Agriculture, Calcutta University, Calcutta 700 0\ 9, India Agropedology, 2001, 1I, 71-77 Forms of acidity and lime requirement of some Alfisols A.K. Dolui and S. Mehta Department of Agricultural Chemistry and Soil Science, University College of Agriculture, Calcutta

More information

Lab Day and Time: Instructions. 1. Do not open the exam until you are told to start.

Lab Day and Time: Instructions. 1. Do not open the exam until you are told to start. Name: Lab Day and Time: Instructions 1. Do not open the exam until you are told to start. 2. This exam is closed note and closed book. You are not allowed to use any outside material while taking this

More information