Managing CBM Product Water A Learning Process With Outcomes James W. Bauder Krista E. Pearson Department of Land Resources & Environmental Sciences Montana.

Slides:



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

Screening for Salt Tolerant Forage Species Conducted by Allison Levy, Undergraduate Under the Direction of Dr. James Bauder, Professor.
Coastal soils: Issues with salinity
Pasture Plant Selection & Grazing Management T.C. Griggs Dept. Plants, Soils, & Biometeorology.
Layout. Soil Texture Describe Topography Topography Maps.
Soil Salinity/Sodicity/Alkalinity and Nutrients
Gregg Carlson, David Clay, Doug Malo, Sharon Clay, and Cheryl Reese.
Background Information Extraction of CBM requires withdrawal of large amounts of water from coal seams containing methane. Projections call for disposal.
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.
Irrigation and Water Quality Section F SWES 316.
Soil Science.
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.
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.
Formation and Characteristics of Hawaii’s Soils
Water Quality Standards for Protection of Irrigated Agriculture in the Powder River Basin Bob Bukantis MT Dept Environ Quality.
Walker River Basin Project Water PlantSoil Interactions Interactions.
Dynamics of Product Water Chemistry & Defining Native Wetland Species Salt Tolerance and Water Use Rates Holly Sessoms.
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
Hailin Zhang Department of Plant and Soil Sciences Oklahoma State University Soil Physical and Chemical Quality and Management in Organic Production.
Potential effects of CMB product water on soil, water, plants, and land resources Kristin Keith James Bauder Dept of Land Resources & Environmental Sciences.
Exchange Reactions Cation exchange Salt/Sodium Affected Soils Acid Soils Lecture 5.
Effects of Saline-Sodic Water on Soil Chemical and Physical Properties Kim Hershberger.
Soil Acidity and pH Causes, remediation, and measurement.
Salinity and Sodicity Management Water or soil with salinity and/or sodicity levels sufficiently elevated to have the potential to have adverse effect.
NWF 3/1/03, Blgs Facts about CBM and water Extraction of CBM requires withdrawal of water from coal seams containing methane. Projections call for disposal.
ASSESSMENT OF WATER QUALITY FOR IRRIGATION: A CASE STUDY IN PUNJAB AMINA MUMTAZ Senior Scientific Officer PCSIR Laboratories Complex, Lahore.
CLM Importance of water Turfgrasses composed of 75-85% water by weight Turfgrasses begin to die if the water content drops below60 to 65% by weight for.
Changes in Spoil Electrical Conductivity (EC) and Sodium Adsorption Ratio (SAR) Following Irrigation at a Mine Site in Northwestern New Mexico Steven Perkins,
Soils 102 – Chemical properties. It’s more than just salt...
Soil Salinity Saline Soil Solution Cation Exchange and Colloidal Phenomena Mineral Weathering Boron Chemistry Irrigation Water Quality.
In arid and semi-arid regions, agriculture is limited by the availibility of suitable irrigation water. Groundwater is the main source of irrigation and.
Situation  Drought, competition, urban growth, declining ground water levels, and evolving water laws and policy are contributing to decreasing supplies.
Chapter 11 - Soil pH and Salinity
How soils supply plant nutrients An Introduction to Soil Chemistry
Soils!.
Soil Electrical Conductivity
Exchange Reactions Cation exchange Acid Soils Salt/Sodium Affected Soils Lecture 5.
1.Freshwater, Marine and Brackish Water Resources 2. Freshwater pollution.
Surface Chemistry. Topics 1.Soil Minerals 2.Soil Adsorption Phenomena 3.Interaction of Water – Clay Minerals 4.Inorganic and Organic Solute Adsorption.
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.
Virtual Academy for the Semi Arid Tropics Course on Insect Pests of Groundnut Module 3: Soils and Climatic requirements After completing this lesson, you.
Sodicity and Salinity Kristie Watling NRW, Toowoomba Ph:
Next End.  Mango grows on wide range of soils, such as lateritic, alluvial, sandy and sandy loam.  Although it grows well in high to medium fertile.
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.
LWR 107 Soils in Dry Regions SOIL ALKALINITY. Causes of Alkalinity: Natural Vs Anthropogenic Characteristics and Problems of Alkaline Soils Development.
U.S. Department of the Interior U.S. Geological Survey Monitoring Surface-Water-Quality in the Tongue River Watershed of Montana and Wyoming Stacy Kinsey.
Coalbed Methane Assessment and Analysis of Produced Water Disposal Options, Northern Cheyenne Reservation, Montana Project FEW Shaochang Wo, Principal.
LANGDON REC GROUNDWATER MANAGEMENT PROJECT OVERVIEW Naeem Kalwar Extension Area Specialist/Soil Health.
Soil Salinity Management Through Cropping Systems
ADDRESSING SOIL ALKALINITY, SALINITY AND SODICITY
Rich Koenig WA State University Phosphorus source effects on dryland winter wheat in eastern Washington Final report.
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.
Soil Salinity.
Soil Water Management Through Cropping Systems Chris Augustin NDSU Soil Health Extension Specialist
MANAGEMENT OF POOR QUALITY WATER FOR IRRIGATION
SOIL AND WATER QUALITY FOR AGRICULTURE
Exchange Reactions Cation exchange Acid Soils
Salinity Demonstrations
Importance of water Turfgrasses composed of 75-85% water by weight
IN THE NAME OF ALLAH, THE COMPASSIONATE, THE MERCIFUL
Chapter 4 Section 2.
Montana Agronomy Seed Identification Study Guide
Presentation transcript:

Managing CBM Product Water A Learning Process With Outcomes James W. Bauder Krista E. Pearson Department of Land Resources & Environmental Sciences Montana State University - Bozeman

Background Information Extraction of CBM requires withdrawal of large amounts of saline- sodic water from coal seams containing methane. Projections call for disposal or management of one quarter million acre- feet of product water annually in the Powder River Basin.

Coal bed methane development is neither new nor confined to the Powder River Basin. Photo courtesy of Dudley Rice, U.S. Geological Survey

Objectives CBM Product Water – What does it look like? What are the interactions between CBM product water and the landscape? Can we effectively manage CBM product water?

CBM Product Water – What does it look like? The common signature of coal bed methane product water is salinity x sodicity.

Wildcat Creek, Campbell County, WY – Tributary to Little Powder River

What is saline water and why is it considered saline? Saline water has a relatively high concentration of dissolved salts. Salinity of water is referred to in terms of total dissolved solids (TDS). –Salinity is estimated by measuring the electrical conductivity (EC) of water. The U.S. Department of Agriculture defines water with an EC greater than 3.0 dS/m as saline.

What is sodic water and why is it considered sodic? The sodicity of water is expressed as the sodium adsorption ratio which is: Sodic water is any water with a SAR greater than 12. Sodic water is not necessarily saline.

Chemistry of CBM Product Water upon Surface Dispersal Holly Sessoms MSU Graduate Research Objective: Determine the behavior of chemistry of CBM product water in stream channels.

CBM Product Water Chemistry CBM product water is bicarbonate rich and under pressure in coal seams. When product water is exposed to the atmosphere, discharged into surface water or applied to soil, sodium bicarbonate undergoes the following reaction: NaHCO 3 H + + CO Na +

CBM Product Water Chemistry Free carbonate (CO 3 -2 ) in solution is now available to bind with calcium in the surface water or soil to form calcium carbonate, i.e., limestone or calcite. Ca HCO 3 - CaCO H CO 2

CBM Product Water Chemistry The dissolution of sodium bicarbonate (NaHCO 3 -) also causes pH to increase with the formation of sodium hydroxide (NaOH): Na + + H + CO 3 CO 2 + Na + +OH -

CBM Product Water Chemistry In summary, sodium bicarbonate-rich CBM product water will initiate the precipitation of calcium carbonate causing: SAR will increase EC values may decrease slightly pH will increase

CBM Product Water Chemistry In a laboratory experiment at MSU, water qualities 6, 7, and 8 with shown initial pH, EC, and SAR values were exposed to the atmosphere for a 9 day period. Initial pH, EC, and SAR reflect changes in CBM product water below the outfall point.

Change in water chemistry for three water qualities over a 9 day time period ( subject to evapoconcentration). Initial pH Final pH Initial EC Final EC Initial SAR Final SAR % Change EC % Change SAR WQ WQ WQ Average % Change

Soil Chemistry Responses to Saline-Sodic Water Kimberly Robinson MSU Graduate Research Objective: Determine how soils which may be subjected to irrigation will react with repeated wetting with saline-sodic water.

Soil Chemistry Responses to Saline-Sodic Water More than 4 dozen soil materials were collected at sample sites within the Powder River Basin. The samples were leached with various water qualities and soil chemical changes were assessed.

Irrigation Simulation Conditions Water Quality –Powder River EC = 1.6 dS/m SAR = 4.5 pH = 8.0 –CBM Product Water EC = 3.1 dS/m SAR = 13.0 pH = 8.0 Irrigation Treatment –Powder River: 1x 5x 5x then distilled water –CBM Product Water: 1x 5x 5x then distilled water

What are the common difficulties with the use of sodic water for irrigation? Use of sodic water for irrigation can be risky business on soils having significant amounts of swelling clay. On such soils: –Sodium changes soil physical properties, leading to poor drainage and crusting, which can affect crop growth and yield. –Irrigation with sodic water on sandy soils does not cause crusting and poor drainage. However, if the water is saline-sodic, it may affect crop growth and yield.

Effect of EC and SAR of applied water on relative hydraulic conductivity (Source: Shainberg and Letey, 1984).

Suggested range in EC and SAR of irrigation water for various soil textures Soil TextureEC range (mmhos/cm) SAR upper limit FloodSprinklerFloodSprinkler Very Coarse sand, loamy sand Coarse sandy loam Medium loam, silt loam Medium fine clay loam, sandy clay loam Fine Silty clay loam, sandy clay, clay, silty clay Source: Western Fertilizer Handbook

1. Thresholds for irrigation.

What are the common problems or difficulties with the use of saline water for irrigation? Crop production becomes a problem as salts accumulate in the root zone high enough to negatively affect plant growth. Excess soluble salts in the root zone restrict plant roots from withdrawing water from the surrounding soil.

Tolerant EC > 10 Semi-Tolerant EC = 4-10 Sensitive EC < 4 CropsBarley Sugarbeet Sunflower Wheat Oats Corn Safflower Potato Field Bean Peas Lentils ForagesTall wheatgrass Bearless wildrye Altai wildrye Slender wheatgrass Western Wheatgrass Russian wildrye Barley Sweetclover Alfalfa Tall Fescue Wheat (hay) Orchardgrass Cicer milkvetch White clover Red clover Ladino clover Alsike clover Meadow foxtail Crop Tolerance to Saline Water

Salinity & Sodicity Tolerance of Selected Plant Species of the Northern Cheyenne Reservation Nikos J. Warrance MSU Graduate Research Objective: Understand how native and culturally significant plant species would respond to increases in salinity and sodicity.

Tolerance and/or sensitivity of selected plants on the Northern Cheyenne Reservation to salinity, sodicity, and flooding Understand how native and culturally significant plants would respond to increases in salinity and sodicity. A list of native and culturally significant plant species was obtained from the Department of Environmental Protection, Northern Cheyenne Tribe. A thorough search of references dealing with salinity, and sodicity tolerances for the plants in question was then undertaken.

Examples of culturally significant plant species of the Northern Cheyenne Reservation Sensitive (EC < 2 dS/m, SAR –June/Service Berry –Red Osier Dogwood –Red Shoot Goose Berry –Chokecherry –Wild Plum –Quaking Aspen –Leafy Aster –Red Raspberry Moderately Sensitive (EC 2-4 dS/m, SAR <8) –Common Spikerush –Field Horsetail –Horsemint –Sweet Medicine –Sandbar Willow –Snowberry –Cattail –Sweet Grass –Saw Beak Sedge –Stinging Nettle –Western Yarrow

Recommended Wetland Species and Aggressive Invaders Dry/moist transition area species include: Canada wildrye (Elymus canadenisis) Slender wheatgrass (Elymus trachycaulus) Western wheatgrass (Pascopyrum smithii) Tall wheatgrass (Thinopyrum ponticum) Native and survivors: Inland saltgrass (Distichlis spicata) Prarie and Alkali cordgrass (Spartina pectinata and gracilis) Baltic rush (Juncus balticus) Nuttalls alkaligrass (Pucinellia nuttalliana) Foxtail Barley (Hordium jubatum) Wet area and in channel survivors or invaders include: American bulrush (Scirpus americanus) Sea Coast bulrush (Scirpus maritimus) Baltic Rush (Juncus balticus)

Screening for Salt Tolerant Forage Species Allison Levy MSU Undergraduate Research Objective: To determine the survivability and early plant biomass production of sixteen different forage species irrigated with water qualities that have been chosen to represent conditions of water surface supplies that could result from coal bed methane development.

Common NameScientific Name CornZea mays AltaiElymus angustus Tall WheatgrassAgropyron elongatum Crested WheatgrassAgropyron cristatum KochiaKochia scorparia SorghumBicolor (L.) moench Intermediate WheatgrassAgropyron intermedium Newhly WheatgrassElyrtigia repens x Pseudoroegneria spicata Tall FescueFestuca arundinacea Paiute OrchardgrassDactylis glomerata L. Slender WheatgrassAgropyron trachycaulum Perennial RyegrassLolium perennal ValierHordeum valier SugarbeetsBeta vulgaris L. Hi Mag Tall FescueFestuca arundinacea hi mag 2nd Gen. AlfalfaMedicago sativa Species Used in Screening for Salt Tolerance

Common NameScientific Name Tall fescueFestuca arundinacea Intermediate wheatgrassAgropyron intermedium Slender wheatgrassAgropyron trachycaulum AltaiElymus angustus SorghumBicolor (L.) moench CornZea mays Valier hay barleyHordeum valier The Short List The short list consists of eight forage species that were chosen for a long-term experiment to assess forage biomass production in greenhouse conditions.

Summary: Lessons Learned Sustainable CBM product water management requires rigorous monitoring and coordinated management. The essential requirements include: –Soil, water, and plant baseline information. –Quantity and quality of CBM product water. –Rigorous monitoring at all points. –Coordinated water management with multiple strategies.