Cation Exchange Capacity

Empty Planting Trays on Rack

Fine Wet Processed Charcoal Settling in Flask

Bamboo Feedstock

Softwood Chip Feedstock

Charcoal Production in Woodgas Stoves

Charcoal Grades

Char Measurement

Amended Pots Prior to Mixing

Pots Mixed and Seeds Sown

 First Watering: 8/11/08

Growth After 9 Days

Wheat and Peas Seperated to Avoid Shading

Some design features below:
Exploring interaction effects of feedstock type, soil, char application
rate, crop species, char size, fertilization, and mycorrhizal fungi.
No repetition (n=1), this loses the ability to assign a statistical
significance level to results, but allows more interactions (96 unique
combinations, 96 pots) to be tried given limited resources.

Charcoal produced in WoodGas stoves.
Char yield 12-18% (char mass/air dry biomass mass) (ie not adjusted to conventional dry weight yield unit, yet).
Fine Char - Blended and sieved to 230 mesh (<63 micron).
Coarse Char - Blended and sieved to between ~24 mesh - 8 mesh.
Fertilizer - 4-4-4 NPK Organic (bone meal, feather meal...)
Potting Soil - Potting Mix
Sandy Soil - Mixture of Horticultural Sand and Sandy Loam from Central Valley

Pots arranged in random spatial order (to randomize light/watering variation). Trays rotated to limit effects of light/watering variation.
Automatic drip emitter watering. Pots grown in enclosed cage outdoors.

Blocks - ( 8 pots/block)
    Fertilizer {Yes,No}
    Plant {Wheat, Pea}
    Soil {Sandy, Potting}

Blocks - (12 blocks * 8 pots/block = 96 pots)
    B1 -    Char (0 g)
    B2 -    Char (1 g, Pine, Fine)
    B3 -    Char (1 g, Pine, Coarse)
    B4 -    Char (1 g, Bamboo, Fine)
    B5 -    Char (1 g, Bamboo, Coarse)
    B6 -    Char (5 g, Pine, Fine)
    B7 -    Char (5 g, Pine, Coarse)
    B8 -    Char (5 g, Bamboo, Fine)
    B9 -    Char (5 g, Bamboo, Coarse)
    B10 -   Char (0 g) + Mycorrhizae
    B11 -   Char (5 g, Pine, Coarse) + Mycorrhizae
    B12 -   Char (10 g, Pine, Coarse)
 

POTENTIAL FOR PYROLYSIS CHAR TO AFFECT SOIL MOISTURE AND NUTRIENT STATUS OF A LOAMY SAND SOIL
J.W. Gaskin, Adam Speir, L.M. Morris, Lee Ogden, Keith Harris, D. Lee, and K.C Das, Proceedings of the 2007 Georgia Water Resources Conference, held March 27–29, 2007, at the University of Georgia.

Abstract.

Pyrolysis of biomass for hydrogen fuel and bio-oil produces a char byproduct. There is evidence that land application of char may increase soil water holding capacity and the ability of the soil to retain nu-trients. Increases in these soil characteristics could be beneficial to plant growth as well as improving water quality. Chars produced under different conditions and from different feedstocks have different characteristics. Of the common feedstocks tested, peanut hull char con-tained higher nutrients and had a higher cation ex-change capacity than pine chip, pine bark, or hardwood chip chars. Preliminary moisture release curve data from a Tifton loamy sand indicated moisture holding capacity may be increased at very high rates of char addition. Soil moisture was periodically measured dur-ing the growing season in a field study of microplots amended with peanut hull and pine chip pellet char. Although the average soil water content of the plots amended at 22 Mg ha-1 was higher than the control, dif-ferences in volumetric water content were only signifi-cant on one date.

Soil Organic Carbon
Jan Skjemstad, CRC Greenhouse Accounting

In Summary

Soil OC is a significant source and sink of atmospheric CO2

Soil is a complex, biologically active medium

Soil OC is not one material

Changes in SOC can be measured directly or can be modelled

The C sink value of soils is limited BUT increasing and maintaining SOC has many benefits for improved productivity and soil resilience

Characterization of Pyrolysis Char for Use as an Agricultural Soil Amendment
Keith Harris1, Julia Gaskin1, Leticia Sonon2, and K.C. Das1
1Dept. of Biol. & Ag. Eng., 2AESL, College of Ag & Env. Sci University of Georgia, Athens, GA

Introduction:
The Southeastern Coastal Plain in the United States is a major agricultural production area; however, soils are typically low in cation exchange capacity (CEC), nutrient content, and organic carbon content. For example, Tifton

Soil Chemical Properties Influenced by Water-Washed Charcoal: Abiotic and Biotic Processes
Chih-Hsin Cheng, Johannes Lehmann and Janice Thies, Department of Crop and Soil Sciences, Cornell University

Introduction
improving soil properties by using charcoal residues, including organic carbon and ashes. High content
of the base ions in the ashes could lead to increase the pH and strongly affect the study results. The

A Flat Kiln and Utilization of Sawdust Charcoal
pdf requires Japanese font
Project Description
Building a Flat Kiln