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ARS Home » Pacific West Area » Kimberly, Idaho » Northwest Irrigation and Soils Research » Research » Publications at this Location » Publication #309392

Research Project: Soil and Water Conservation for Northwestern Irrigated Agriculture

Location: Northwest Irrigation and Soils Research

Title: Designer, acidic biochar influences calcareous soil characteristics

Author
item Ippolito, James
item Ducey, Thomas
item Cantrell, Keri
item Novak, Jeffrey - Jeff
item Lentz, Rodrick - Rick

Submitted to: Chemosphere
Publication Type: Peer Reviewed Journal
Publication Acceptance Date: 6/2/2015
Publication Date: 6/12/2015
Publication URL: http://handle.nal.usda.gov/10113/61135
Citation: Ippolito, J.A., Ducey, T.F., Cantrell, K.B., Novak, J.M., Lentz, R.D. 2015. Designer, acidic biochar influences calcareous soil characteristics. Chemosphere. Available: http://dx.doi.org/10.1016/j.chemosphere.2015.05.092.

Interpretive Summary: Increasing amounts of a low-temperature designer biochar were added to an eroded calcareous soil and destructively sampled over time to observe potential changes in the soil physicochemical status. Soil pH and nitrate-nitrogen decreased, while soil water content, carbon, microbial activity, and plant-available zinc, manganese, and phosphorus increased with increasing biochar application rate; micronutrient availability tended to decrease over time likely due to the precipitation of insoluble mineral species. Our results showed that there is promise in designing a biochar to improve the quality of eroded calcareous soils with concomitant increases in soil microbial activity.

Technical Abstract: An acidic (pH 5.8) biochar was created using a low pyrolysis temperature (350 degrees celsius) and steam activation to potentially improve the soil physicochemical status of an eroded calcareous soil. Biochar was added at 0, 1, 2, and 10 percent (by weight) to an eroded Portneuf soil (coarse-silty, mixed, superactive, mesic Durinodic Xeric Haplocalcid) and destructively sampled at 1, 2, 3, 4, 5, and 6 month intervals. Soil was analyzed for volumetric water content, pH, nitrate-nitrogen, ammonium-nitrogen, plant-available iron, zinc, manganese, copper, and phosphorus, organic carbon, carbon dioxide respiration, and microbial enumeration via extractable DNA and 16S rRNA gene copies. Soil water content increased with biochar application regardless of rate; the response was consistent over time. Soil pH decreased between 0.2 and 0.4 units, while plant-available zinc, manganese, and phosphorus increased with increasing biochar application rate. Micronutrient availability tended to decrease over time likely due to the precipitation of insoluble mineral species. Increasing biochar application raised the soil organic carbon content and it remained elevated over time. Increasing biochar application rate also increased respired carbon dioxide, yet the carbon dioxide released decreased over time. Soil nitrate-nitrogen concentrations significantly decreased with increasing biochar application rate likely due to microbial immobilization. Depending on application rate, biochar produced a 1.4 to 2.1-fold increase in soil DNA extracted and 1.4- to 2.4-fold increase in 16S rRNA gene abundance over control soils, suggesting microbial stimulation and a subsequent burst of activity upon biochar addition. Our results showed that there is promise in designing a biochar to improve the quality of eroded calcareous soils with concomitant increases in soil microbial activity.