CATION EXCHANGE CAPACITY

Slides:



Advertisements
Similar presentations
Soil Samples Analyses and Interpretation. PPM parts per million average weight of 6 inch soil =2 million pounds 1 ppm = 2 pounds / acre.
Advertisements

Soil Loam: a mixture suitable for growing plants Components:
Cation Exchange Capacity in Soils
Soil Fertility and Nutrient Bioavailability Sponsored by the DEST program China Higher Education Strategic Initiatives © The University of Adelaide.
Bahan Kajian MK. Dasar Ilmu Tanah KTK & KETERSEDIAAN HARA Smno.agroekotek.fpub.nop2013.
Class evaluations.
Interest Approach Collect samples of growing media. Some suggestions are water, sand, peat moss, gravel, garden soil, potting mix, etc. Have the students.
Soil Chemical Properties
UNDERSTANDING AGRONOMY. Plant Nutrients and Fertility Objectives Identify essential nutrients for plant growth; Identify essential nutrients for plant.
Environmental Processes Fundamental processes in soil, atmospheric and aquatic systems 2.i Ion exchange.
Nutrient management for organic vegetable production in NC Part I.
Lecture 12 b Soil Cation Exchange Capacity
SOIL CHEMISTRY SOIL pH A measure of the degree to which the soil is Acidic or Basic; also known as... Soil Reaction.
Soil Acidity and Nutrients
LECTURE 10 Introduction to some chemical properties of soils : Factors affecting plant growth (2)
How nutrients, soil particles and chemistry fit together
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.
Mineral Nutrition (chapter 4). Mineral Nutrition How plants acquire and use mineral nutrients 1. Why is mineral nutrition important? 2. What are the essential.
Calculating wet topsoil pile weight Calculate the moisture content (w): w = [(g water) / (g dry soil)] x 100 = % Calculate dry topsoil weight using Db.
Nutrients, pH and Fertility Topic 2035 Anna Blight.
Overview of Soil Properties for Crop Production By J.G. Mexal Department of Agronomy & Horticulture New Mexico State University.
HORT 301 – Plant Physiology October 5, 2007
Mineral Nutrition Plant life cycle
Visual comparison of common silicate clays
The Effect of Non-Composted and Composted Soil on Nutrient Concentrations in Green Beans By Nicol, Scott, and Jenn.
Environmental chemistry
Soil Buffering and Management of Acid Soils. pH pH = - log (H + ) If (H + ) = 1 x mol/L (H + ) = mol/L pH = - log (1 x ) pH = - (-3)
Thomas Obreza Soil and Water Science Dept. Univ. of Florida Soil Fertility and pH.
Soil 50% pores and 50% solids
Cation Exchange Definition: substitution of ions in solution for those held by a mineral grain. Associated with many different types of materials found.
Plant Nutrition. Mineral Nutrition How plants acquire and use mineral nutrients 1. Why is mineral nutrition important? 2. What are the essential mineral.
Soils NR 200.
Rock Weathering and Soil Mineralogy. Physical Weathering……
How soils supply plant nutrients An Introduction to Soil Chemistry
PRESENTED BY AKHTAR MEHMOOD ROLL # DEPARTMENT OF BOTANY M.PHIL BOTANY FINAL SEMESTER.
GOLF COURSE AND TURF SOLUTIONS PRESENTED BY GAVIN OLSEN.
Chapter 2 The Soil.
Soils All terrestrial life is ultimately a product of the soil in which primary producers grow.All terrestrial life is ultimately a product of the soil.
Soil Properties Carolina Medina Soil & Water Science Dept. University of Florida.
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.
Chapter 2 The Chemical Context of Life. Comment u Much of this chapter should be review from your chemistry class. The material should not be brand new.
What are the types of growing media used in floriculture production? The health and quality of horticultural crops rest largely with the growing medium.
SOIL CHEMISTRY.
Surface Chemistry. Topics 1.Soil Minerals 2.Soil Adsorption Phenomena 3.Interaction of Water – Clay Minerals 4.Inorganic and Organic Solute Adsorption.
West Hills College Farm of the Future The Precision-Farming Guide for Agriculturalists Chapter Four Soil Sampling and Analysis.
Physical Science Applications in Agriculture Unit Physical Science Systems.
Ionic Compounds. Formulas for Ionic Compounds A chemical compound must have a net charge of zero. In a chemical formula showing the combining of ions.
Chapter 2 The Chemical Context of Life. Comment u Much of this chapter should be review from a basic chemistry course. Much of the material is unlikely.
Reactions of Aluminosilcates
SOIL FERTILITY INTRO TO SOILS CH 10. SOIL FERTILITY Ability of soil to supply nutrients for plant growth Readily Available – soil solution Not Readily.
Soil colloids. CHEMICAL PROPERTIES OF SOIL: Soil Colloids cat ion Exchange organic matter / Organic carbon Carbon –Nitroge ratio Soil fertility Soil reaction.
Basic Soil Plant Relationships Fundamentals of Nutrient Management Training Course Dec. 14, 2005 Jim Gorman West Virginia University.
SOIL REACTIONS, SOIL ACIDITY SOIL ALKALINITY, CONDUCTIVITY, REDOX POTENTIAL.
SOIL FERTILITY.
Integrated Nutrient Management (Nutrient Essential for Plants) A Series of Lecture By Mr. Allah Dad Khan.
Hydroponic Science Supplying Nutrients to Crops
Micronutrient elements
Interpreting Georgia Soil Test Reports
Soil Chemistry.
Plant Fertility.
Soil Nutrients C, H, O, from the air, water The rest from the soil.
Soil Science & Management, 4E
Physical Science Applications in Agriculture
Interest Approach Collect samples of growing media. Some suggestions are water, sand, peat moss, gravel, garden soil, potting mix, etc. Have the students.
Ch. 4: Soil Water, Plant Nutrition, Soil Symbioses
Plant Nutrition.
CATION EXCHANGE CAPACITY
Determination of Soil Acidity
Agricultural Ecology.
Ch. 4: Soils, Nutrition etc.
Presentation transcript:

CATION EXCHANGE CAPACITY and PLANT NUTRITION

Cation Exchange Capacity (CEC) Clay Particles and Humus affect chemical properties of soil complex structures with many negative charge sites negative charge sites attract positive ions called cations

+ attract cations from soil solution+ CEC Negative charge sites are referred to as . . . Cation exchange sites + attract cations from soil solution+

CEC Adsorption Force of attraction is called: similar to force of a magnet holding iron filings

CATION ADSORPTION

CEC Cations can move on and off particles . . . when one leaves, another replaces it This process is called cation exchange, and cations involved are said to be exchangeable http://www.une.edu.au/~agronomy/SSCATXCH.dcr

CEC The number of sites that a colloid (small particle) of charged clay or humus (micelles) contains is measured by the: Cation Exchange Capacity expressed in mEq/100g (older unit) or cmolc/kg

CEC may range from: 2.0 mEq/100g for sand to > 50 mEq/100g for some clays and humus 100-300 mEq/100g under certain soil conditions

CEC How fertile can a soil be? Does applying more fertilizer always provide more nutrients to plants? How much of the CEC is actually filled with cations?

CEC The proportion of the CEC occupied by basic (+) nutrients such as Ca, Mg, K, Na, is called: Percent Base Saturation and is an indication of the potential CEC of a given soil

CEC Estimations that > 99% of cations in soil solution are adsorbed . . . does not mean that percent base saturation is 99%

CEC Example: A soil with CEC of 10 mEq/100g has 6 mEq/100g of bases (Ca, Mg, K, Na) occupying exchange sites What is the percent base saturation of the soil?

CEC 6 mEq/100g bases 10 mEq/100g sites = 60 % base saturation

Cation Exchange is determined by: CEC Cation Exchange is determined by: 1) strength of adsorption 2) law of mass

CEC Strength of adsorption is as follows: H+ and Al3+ > Ca2+ > Mg2+ > K+ > NH4+ > Na+

CEC Law of Mass the more of one ion available, the greater the chance of adsorption

NUTRITION There are at least 17 elements recognized as essential nutrients for plants; we will recognize 18 elements: C, H, O, P, K, N, S, Ca, Fe, Mg, Mn, Mo, Cl, Cu, Zn, B, Co, Ni

NUTRITION Nutrients grouped into 2 categories according to the relative amount used by plants: Macronutrients – major elements; large amounts Micronutrients – minor elements; small amounts Both are essential for optimal plant production

ROOT HAIR ABSORPTION

NUTRIENTS REPLACE CATIONS

NUTRITION Note: C, H, O . . . essential elements not considered in nutritional studies; Why?

NUTRITION > 95% of plant dry wt. from C, H, O; (balance from macro, micro and other elements)

NUTRITION Except for C, H, O . . . - Nitrogen (N) is present in greatest concentrations; - Plants respond readily to Nitrogen (N)