Irrigation and Water Quality Section F SWES 316.

Slides:



Advertisements
Similar presentations
IN THE NAME OF ALLAH, THE COMPASSIONATE, THE MERCIFUL.
Advertisements

Coastal soils: Issues with salinity
CE 547 Softening. What is Hardness Hardness is –the ability of the water to consume excessive amounts of soap before foaming –OR the ability of the water.
Urban Landscape Irrigation with Recycled Wastewater: Water Quality and Salinity Issues Yaling Qian Colorado State University.
Oak Hill Case Soil Chemical Problems. SALT - RELATED PROBLEMS Ion Toxicities Ion Imbalances Soil Permeability Water Deficits.
Layout. Soil Texture Describe Topography Topography Maps.
1 Weak Acids and Bases A weak acid or base is an acid or base that partially (less than 100%) dissociated in water. The equilibrium constant is usually.
Equilibrium Chemistry
Solubility of CO2 and Carbonate Equilibrium
Soil Salinity/Sodicity/Alkalinity and Nutrients
LECTURE 11 Introduction to some chemical properties of soils : Factors affecting plant growth (3)
Phosphorus and Potassium. How is P managed? Key to managing soil and fertilizer P: Knowledge of whether or not the level of soil solution P is adequate.
Chapter 14.  Equilibrium occurs when there is a constant ratio between the concentration of the reactants and the products. Different reactions have.
Gregg Carlson, David Clay, Doug Malo, Sharon Clay, and Cheryl Reese.
Electrical conductivity, EC A quick method to measure the salinity of water. EC is approximately one-tenth of the total dissolved cation, or anion concentration.
Soil Structure: The Roles of Sodium and Salts
5. Buffering capacity Soils high in SOM and clay minerals are more resistant to change in pH Sandy soils and highly weathered soils are least buffered.
Class evaluations.
The Punic Wars –Case for Salt in Soils “After the third punic war, the Romans stormed the town and the army went from house to house slaughtering the inhabitants.
Introduction to Groundwater Chemistry October 04, 2010.
Soil and Water Salinity Dissolved salts decrease the osmotic potential of soil water (which lowers the Total Soil Water Potential) a decrease in soil solution.
Soil Science and Management, 4E
SOIL CHEMISTRY SOIL pH A measure of the degree to which the soil is Acidic or Basic; also known as... Soil Reaction.
Reclamation of salt- affected soils
Soil Acidity and Nutrients
E NVIRONMENTAL CHEMISTRY E 12. water and soil. W ATER AND SOIL Solve problems relating to the removal of heavy- metal ions, phosphates and nitrates from.
Soil Acidity and pH Causes, remediation, and measurement.
ASSESSMENT OF WATER QUALITY FOR IRRIGATION: A CASE STUDY IN PUNJAB AMINA MUMTAZ Senior Scientific Officer PCSIR Laboratories Complex, Lahore.
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)
Soil Testing and Analysis Nutrient Management Basics
PLANNING PHASE. “ A row crop drip system does not make a farming operation good. On the contrary, one needs to START with a farming operation and then.
Soil Salinity Saline Soil Solution Cation Exchange and Colloidal Phenomena Mineral Weathering Boron Chemistry Irrigation Water Quality.
FRUIT GROWERS LABORATORY, INC. Darrell H. Nelson Horticulturalist.
In arid and semi-arid regions, agriculture is limited by the availibility of suitable irrigation water. Groundwater is the main source of irrigation and.
Chapter 18 – Other Aspects of Aqueous Equilibria Objectives: 1.Apply the common ion effect. 2.Describe the control of pH in aqueous solutions with buffers.
Chapter 11 - Soil pH and Salinity
Improving Irrigation & Nutrient Efficiency Improving Irrigation & Nutrient Efficiency.
IV. Water Chemistry A. pH, hardness, and other ionic compounds and gases affecting water quality.
Water Test Interpretation Mike Kizer OSU Extension Irrigation Specialist Ca ++ Na + Na + Cl - Cl - SO 4 = K + Mg ++ HCO 3 - CO 3 = NO 3 -
Soil. Chemistry Review Cation: atom that forms a positive charge (example: Ca +2 ) anion: atom that forms a negative charge (example: S -2 )
Acid-Base Equilibria (Buffers ) Green & Damji Chapter 8, Section 18.2 Chang Chapter 16 Copyright © The McGraw-Hill Companies, Inc. Permission required.
Soil Electrical Conductivity
Introduction Proper nutrition at nursery stage is important for desired growth and berry production in grapevine. There are 13 mineral nutrients found.
Solubility Equilibria
Exchange Reactions Cation exchange Acid Soils Salt/Sodium Affected Soils Lecture 5.
Where Does The Water Come From ?. Soil Zone Sand and Gravel Aquifer Limestone or Granite Aquifer Sandstone Aquifer Examples of Variation in Groundwater.
Saline and Sodic Soils Chapter 10. This one. Percent yield on y-axis and increasing level of salinity on x-axis.
Seasonal Effects on Ground Water Chemistry of the Ouachita Mountains Data Interpretation: Drew Lonigro.
Wednesday, March 19 th : “A” Day Thursday, March 20 th : “B” Day Agenda  Homework questions/problems?  Section 14.1 Quiz  Begin Section 14.2: “Systems.
Sodicity and Salinity Kristie Watling NRW, Toowoomba Ph:
You have learnt from the lessons in the earlier Modules that soil properties influence soil health. These soil properties in turn are affected by the agricultural.
Update of the Rationale for the Derivation of EC & SAR Standards Montana Board of Environmental Review May 13, 2011.
MAZHAR ABBAS ag TH Agronomy University Of Agriculture Faisalabad
Soil Chapter 8 Acidic Soils & Salt Affected Soils Pages 229 – 262.
Avocado Irrigation – Special Topics
LWR 107 Soils in Dry Regions SOIL ALKALINITY. Causes of Alkalinity: Natural Vs Anthropogenic Characteristics and Problems of Alkaline Soils Development.
 Greater flexibility in application of fertilizers does not depend on the climatic conditions such as rain and soil condition.  Frequent and small applications.
SOIL REACTIONS, SOIL ACIDITY SOIL ALKALINITY, CONDUCTIVITY, REDOX POTENTIAL.
ADDRESSING SOIL ALKALINITY, SALINITY AND SODICITY
Name: manzoor nabi Course: forestry Roll no: 04 Acidic, Salic, And Alkali Soils MEWAR UNIVERSITY.
Master Seminar on Effect Of Salinity and Alkalinity on Physico-chemical Properties of soil Presented by Hemant Kumar M.sc. (previous) Deptt. of Soil Science.
Irrigation Water Quality & Influence on Crop Production Sam Taylor, March 2016.
MANAGEMENT OF POOR QUALITY WATER FOR IRRIGATION
Soil Chemistry.
Exchange Reactions Cation exchange Acid Soils
Saline Soil.
Saline Soil.
IN THE NAME OF ALLAH, THE COMPASSIONATE, THE MERCIFUL
Chemistry of seawater Salt pH Gases Nutrients.
Presentation transcript:

Irrigation and Water Quality Section F SWES 316

Salt Moves to the Terminus of the Wetting Front!

Border/Flood Irrigation Furrow Irrigation Sprinkler Subsurface drip

Why Water Quality is Important Effects on Soil Salinity Effects on Soil Sodicity Bicarbonate content Toxic ion content Effects on nutrients applied by fertigation

Irrigation and Water Quality When soils are irrigated, the quality of the water used will eventually determine the salinity and sodicity of the soil: Soils will be at least 1.5 times more saline than the water used to irrigate them, unless very high (>20%) leaching fractions are used. The ESP (and SAR) of the soil will eventually equal the sodium adsorption ratio (SAR) of the water.

Irrigation Water Quality Important Measurements: Salinity (measured by EC) Sodium (measured by SAR) Potential toxic ions (Na, Cl, B) Alkalinity or HCO 3 - SAR=

Irrigation Water Hazards Interpreting Salinity Remember that even with excellent management, soil EC will be at least 1.5X that of the water used (except in very coarse-textured soils or very high LF). Crop tolerance varies, however Interpreting sodicity - depends on clay content and salinity

Irrigation Water Hazards Concentrations of toxic ions: Cl - Na + B (H 3 BO 3 ) Bicarbonate - precipitates Ca 2+ from soils, makes Na problems worse.

General Guidelines Degree of Restriction on Use Potential ProblemUnitsNoneSlight to ModerateSevere pHNormal range 6.5 – 8.4 Salinity ECdS/m< – 3.0>3.0 TDSmg/L< – 2,000>2,000 Infiltration SAR=0-3 and EC w => – 0.2<0.2 SAR=3-6 and EC w => – 0.3<0.3 SAR=6-12 and EC w => – 0.5<0.5 SAR=12-20 and EC w => – 1.3<1.3 SAR=20-40 and EC w => – 2.9<2.9 Specific ion effects Sodium Surface irrigationSAR<33-9>9 Sprinkler irrigationmeq/L<3>3 Chloride Surface irrigationmeq/L< >10 Sprinkler irrigationmeq/L<3>3 Boronmg/L< – 3.0>3.0

Specific Guidelines CropEC e EC w LREC e EC w LREC e EC w LREC e EC w LRECw 0%10%25%50%max Date palm % % % %32.0 Fig % % % %14.0 Olive % % % %14.0 Pomegranite % % % %14.0 Grapefruit % % % %8.0 Orange % % % %8.0 Lemon % % % %8.0 Apple % % % %8.0 Pear % % % %8.0 Walnut % % % %8.0 Peach % % % %6.5 Apricot % % % %6.0 Grape % % % %12.0 Almond % % % %7.0 Plum % %2.9 14% %7.0 Blackberry % % % %6.0 Avocado % % % %6.0 Raspberry % % % %5.5 Strawberry % % % %4.0

Controlling Salinity in Irrigated Soils The only way to control salinity in irrigated soils is to __________________________ _________________. If irrigation water EC is <0.75 dS/m, no risk of salt buildup. Normally, the soil is at least 1.5X the salinity of the irrigation water used because ___________________________. leach adequate quantities of water through soil not all water added can leach

Leaching Requirement Definition: The percentage of water (rain + irrigation) applied that must move below the root zone to control salt buildup. Equation:

Notes on LR The LR is the amount of total water that should be applied above crop water use. Can be applied at every irrigation, or only periodically The LR you calculate depends on assumptions. This is a fairly crude method - also consider irrigation system characteristics. LRs above 30% are not very practical.

Other Ways to Live with Salts Keep soils moist - this keeps salt concentrations more dilute. May require frequent irrigation. Drip irrigation !!! Plant seeds on the sides of sloping beds. Salts move with water Use plants that are salt-tolerant

Squash planted on sides of beds to avoid zone of highest salt.

Fun things you can do with EC Estimate total dissolved solids (TDS) EC (dS/m) x 640  TDS (ppm) Estimate osmotic potential of soil solution  o (bars)  EC (dS/m) x (-0.36)

Controlling Sodium The SAR describes the equilibrium relationship between Na, Ca, and Mg. It should be as low as possible. Over time, the ESP of the soil will equal the SAR value of the irrigation water. In order to control Na, a source of ______ must be added to irrigation water. Ca 2+

Irrigation Water Treatment (1)  Regular treatment of irrigation water can help prevent the formation of sodium problems.  Irrigation water can be regularly treated with gypsum to lower SAR of water. Typical rates: lbs/acre-foot water (326,000 gallons)  There is no effective (economical) water treatment to counteract salinity.

What does gypsum do? Poor soil structure Good soil structure Sodium level (SAR) Based on irrigation water analysis

Soil Amendments and Water Treatments Soil application of amendments are used for initial reclamation and long-term maintenance of soil quality. Rates are often large and based on economics. Water treatments are generally intended to alter the chemistry of irrigation water so that no further degradation in soil quality will occur. Rates used for water treatment are usually small and based on solubility and stoichiometry.

Bicarbonate Hazard Excess HCO 3 - causes precipitation of CaCO 3 thus increasing the Na hazard (SAR) of irrigation water

Irrigation Water Treatment (2) Carbonate (CO 3 2- ) and bicarbonate (HCO 3 - ) in irrigation water are detrimental because they: precipate Ca 2+ from soil solution and hasten replacement of Ca 2+ with Na + Treatment of irrigation water with H 2 SO 4 to a pH <6.0 will convert all CO 3 2- and HCO 3 - to CO 2.

Water Quality and Nutrient Management (1) Ammonia Volatilization NH 4 +  NH 3 + H + Addition of NH 4 + fertilizers in alkaline water will encourage this equilibrium toward the right. Solution: acidify water first Water pH % NH 3 volatilized

Water Quality and Nutrient Management (2) Adding NH 3 to irrigation water (as a fertilizer) will raise water pH to This will: Cause NH 3 volatilization Remove Ca and Mg from water by precipitating them as carbonates Can irreversibly plug irrigation systems Solution: Acidify water first

Calcium Carbonate Precipitation 1. High bicarbonate Ca HCO 3 - > CaCO 3 + H 2 CO 3 >H 2 O + CO 2 2.Ammoniated water NH 3 + H 2 O > NH 4 OH NH 4 OH > NH 4 + OH OH- + HCO 3 > CO H 2 O Ca ++ + CO 3 -2 > CaCO 3(s)

Constant H 2 SO 4 injection keeps water pH low and prevents formation of CaCO 3 in the drip lines, and also dissolves some CaCO 3 in the soil, helping to maintain high exchangeable Ca 2+ and low exchangeable Na +.

Water Quality and Nutrient Management (3) Many P fertilizers are not very soluble in water. Adding them to irrigation water high in soluble Ca will lead to precipitation of Ca-phosphates Loss of P Plugging of irrigation system