Carbon remaining (%) 100 12345 Years Biochar Uncharred Biomass Centuries? Millennia? Compost 500+°C Dr. Johannes Lehman – and hydrophobic – it repels water.

Slides:



Advertisements
Similar presentations
Weathering and Soil Test Review.
Advertisements

Biochar amendment to improve soil properties and sequester carbon
Soil.
Soil. organic the top layer of the earths surface, consisting of rock and mineral particles mixed with organic matter.
SOIL.
Biochar Properties Water Absorption Micropore Sponge
Conservation Grassland
product identity & integrity
PHOTO: Bob Cirino, University of Delaware into chlorophyllcarbohydratesphotosynthesis + water = electrolytes Nitrogen, Boron, Iodine Phosphorus, Sulfur,
Lab: Plankton Sampling and Analysis Ventura Pier, Harbor and Estuary.
Bacteria populations show sharp increase after charcoal addition Beijerinckia, Ogawa 1992 residential refuges for micro-organisms Glomalus Margarita germination.
PHOTO: Bob Cirino, University of Delaware into chlorophyllcarbohydratesphotosynthesis + water = electrolytes Nitrogen, Boron, Iodine Phosphorus, Sulfur,
Huma-Char ® and Its Benefits to Agriculture Heating Up Crop Production With an Ancient Soil Amendment Dr. Vladimir Vasilenko (Dr. Humate)- Technical Director.
Click to continue New England Biochar Peter Hirst Orleans, MA Ideal Compost Mike Lombard Peterborough, NH
Soil Composition – What Dirt is Made of
Dirt on Soil. What is Soil? Soil forms as rock is weathered and mixes with other materials on the surface. Soil forms as rock is weathered and mixes with.
What is the dirt on soil?. Soil, is made from rocks that break apart or wear away over many years. This is referred to as weathering. It may take 100.
Soil: A Natural Resource SOL 3.7
LECTURE 10 Introduction to some chemical properties of soils : Factors affecting plant growth (2)
Properties of Soil. Where does soil come from and how does it form? Most soils were originally created through the breaking down (weathering) of the solid.
1 10 pt 15 pt 20 pt 25 pt 5 pt 10 pt 15 pt 20 pt 25 pt 5 pt 10 pt 15 pt 20 pt 25 pt 5 pt 10 pt 15 pt 20 pt 25 pt 5 pt 10 pt 15 pt 20 pt 25 pt 5 pt Category.
Soil Organic Matter and Decomposition. Organic compound + O 2 (or other electron acceptor) CO 2 + H 2 O + energy + inorganic nutrients  a form of respiration.
Remote Sensing for Geologic Applications Soil Properties Mineral and Rock Identification Geomorphology (landforms) Volcanology Coastal Processes Fluvial.
Ch 3 Soil Organic Matter continued.
Arbuscular Mycorrhyzal Fungi produce a Glomalin glue which aggregates small soil particles Fertile Soil is “aggregated” This increases water & air holding.
Soil.
Soil Composition 1/13/12. What determines characteristics of soil? Physical (such as water) Parent material (chemical make-up) Life (biological activity)
SOIL Medium: The soil mixture is the plant’s source for food, water, and support The soil mix will have effect on the health, vitality, and appearance.
The AIR blows naturally – it is not caused by human activity, and it cannot be used up. The power of the AIR drives sailboats. It has been used to.
1 2 pt 3 pt 4 pt 5pt 1 pt 2 pt 3 pt 4 pt 5 pt 1 pt 2pt 3 pt 4pt 5 pt 1pt 2pt 3 pt 4 pt 5 pt 1 pt 2 pt 3 pt 4pt 5 pt 1pt Soil My name is not Dirt My name.
AP Environmental Science Soil Resources (Ch 14) Living in the Environment, 14th edition, G. Tyler Miller.
How soils supply plant nutrients An Introduction to Soil Chemistry
Earth’s Surface is Constantly Changing
Importance & Formation of Soil. Importance of Soil Much of the United States ’ success is due to the productive capacity of the soil – U. S. produces.
Soil, an Essential Natural Resource
Soil! By: Oksanna Loya.
Biochar for Reclamation in the Rocky Mountains: Context, Science and Policy – Can We Find a Nexus that Works Andrew Harley, Tetra Tech, Inc Morgan Williams,
*Compost is a mixture of decayed organic materials decomposed by microorganisms in a warm, moist, and aerobic environment, releasing nutrients.
Soil Respiration Unit: Soil Science. Objectives O Define: soil respiration and soil microbes O Explain the role of soil respiration in determining soil.
Properties of Soil Grade 4.
Soil is a mixture of weathered rock particles and other materials.
Do Now In your own words, describe what soil is and what it’s made up of.
AP Environmental Science Soil Resources Living in the Environment, 14th edition, G. Tyler Miller.
Surface Chemistry. Topics 1.Soil Minerals 2.Soil Adsorption Phenomena 3.Interaction of Water – Clay Minerals 4.Inorganic and Organic Solute Adsorption.
Emerging Environmental Issues Darrell A. Fruth Brooks, Pierce, McLendon, Humphrey & Leonard LLP
Formation of Soil UNIT 5 STANDARDS: STATE OBJECTIVES: NCES 2.1.1, 2.1.3, LESSON 3.
Earth’s Surface Chapter 2 Weathering and Soil
Weathering and Soil Formation Notes. Weathering Two types – Mechanical Weathering Ice Abrasion Wind, Water, Gravity Plants Animals Chemical Weathering.
What are we going to learn…  Soil-Why is it important? Why is it important?  What is soil?  Sand, Silt and Clay  What’s a soil profile?  Horizons?
WEATHERING & SOIL. Weathering  The chemical and physical alterations of rock and other Earth materials at or near earth’s surface, through the action.
What is the dirt on soil?.
How Soil Forms WEATHERING AND SOIL. Soil is the loose, weathered material on Earth’s surface in which plants can grow. WHAT IS SOIL?
Are these examples of weathering, erosion, or both?  1. Ice breaking rock  2. Wind breaking away and moving rock  3. A river moving sediment  4. Tree.
Soil Formation and Composition
What is the best soil for growing plants? Loam soil that is made of almost equal parts of clay, sand, and silt is the best. This texture is important so.
 Essential Question: How does soil form, and what purposes does it serve?  Objectives: 1. Describe the functions of soil 2. Describe the factors of.
Ecosystem Productivity and Soils. Energy Pyramid.
Weathering  It is surface processes that break down rock  Breaks rocks into smaller and smaller pieces  Ex.) Sand, silt, clay  The formation of soil.
Weathering and Soil Formation. What is weathering?
Soil and Climate. Learning Objectives 2)Soil and Climate a)Assess the significance of Solar Radiation to plant growth b)Illustrate the hydrological cycle.
Soils NOT Just Dirt By: Rebekah Triolo. Defining Soil “a natural body consisting of layers (horizons) of mineral and/or organic constituents of variable.
Soil. What is soil? Soil is a mixture of bits of weathered rock, humus, water, and air. Soil is a mixture of bits of weathered rock, humus, water, and.
Table of Contents Rocks and Weathering How Soil Forms
SOIL FERTILITY.
Weatheringand Soil Formation. Rocks and Weathering.
August 2008 Organic Matter What is organic matter Original Power Point Created by Darrin Holle Modified by Georgia Agricultural Education Curriculum Office.
WEATHERING AND SOIL CH 9 8 TH GRADE. 9.1 ROCKS AND WEATHERING WHAT BREAKS DOWN ROCKS? IT’S A HARD ROCK LIFE EROSION PT 1 EROSION PT 2 EROSION VS WEATHERING.
The Effects of Biochar on Plant Growth
The Truth about Soil and Soil Conservation
Soils and their Significance
Presentation transcript:

Carbon remaining (%) Years Biochar Uncharred Biomass Centuries? Millennia? Compost 500+°C Dr. Johannes Lehman – and hydrophobic – it repels water with no biological activity – no microbes Fresh from a burner, biochar is sterile, Biochar isn’t consumed by soil life not affected by weathering, oxidation & digestion – not in months, but decades, even centuries In soil, charcoal breaks down very slowly : Habitat and housing for microbes Substrate : Adsorp nutrient ions (C.E.C. & A.E.C.) Storehouse : Absorb, hold & conserve soil water Sponge Biochar supplies three important soil services: Adding only raw charcoal to soil Fertilizers must be added with charcoal retards plant growth 1 or 2 years is biochar a fertilizer? is biochar a nutrient? Biochar Properties 50 Pyrolysis 10 Humus

PPPParticle size SSSSurface area RRRResidence Time SSSStructural density MMMMicropore density MMMMoisture content WWWWater Absorption IIIIon Adsorption CCCCEC ppppH MMMMicrobial Activity Physical Properties & AEC Biochar Properties PPPParticle size MMMMicropore density WWWWater Absorption CCCCEC & AEC MMMMicrobial Activity

PHOTO: Bob Cirino, University of Delaware Surface area External: square inches vs. square miles Internal: micropores Varied sizes varied purposes: broadcast, seed drill, potting mix, hydroponics Gravel Rice grain Powder & Dust Water soluble: lowest molecular weight Micronize: Nature’s nanotechnology Brittle: easy to crush Dusty: easily blows away Variable: with feedstock Woody vs. Weedy Screen: separate sizes Intimate mix: at cellular and molecular scales Particle Conversion Chart Particle SizeDiameter (microns) Mesh (screen size) Fine Sand Very Fine Sand Silt Clay 2 or less 6000 or more Particle Size Biochar Properties

RRRRecalcitrant Resists chemical & weathering action Resists microbial digestion & decay Sequestration = at least 100 years Dr. David Laird, USDA Tilth Lab: 1600 year half-life  1 to 5% loss Tar & Resins Residues (VOC & PAH) Hydrophobic (oily hydrocarbons)  Vary with production process Temperature: °C (energy only: up to 1500°C) Pressure, Length of Time, Steam Gasification vs. Pyrolysis (burning vs. baking) Torrefication, Fast Pyrolysis, Flash Pyrolysis, Microwave Residence Time Biochar Properties Carbon remaining (%) Years Pyrolysis Composted Biomass Humus Biochar 1−5% 10−15% 35−50%