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This article in JEQ

  1. Vol. 31 No. 4, p. 1323-1328
     
    Received: June 8, 2001
    Published: July, 2002


    * Corresponding author(s): lqma@ufl.edu
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doi:10.2134/jeq2002.1323

Relationship between Compost Stability and Extractable Organic Carbon

  1. L. Wu and
  2. L.Q. Ma *
  1. Department of Soil and Water Science, Univ. of Florida, Gainesville, FL 32611-0290

Abstract

Establishing a simple yet reliable compost stability test is essential for a better compost quality control and utilization efficiency. The objective of this study was to examine the relationship between extractable organic carbon (OC) and compost stability based on 18 compost samples from five composting facilities. The compost samples were extracted sequentially with water for 2 h [water(2h)] and 0.1 M NaOH for 2 and 24 h [NaOH(2h) and NaOH(24h), respectively]. The extractable OC was further separated into fulvic acid (FA) and humic acid (HA) fractions by adjusting the pH to <2. The mass specific absorbance (MSA) of OC in the six fractions was measured. Compost stability was estimated with a CO2 evolution method. The extractable OC concentration was influenced by the total volatile solids and decreased with curing time for compost with a high level of extractable OC. The OC levels in each fraction were significantly correlated (p < 0.05) to each other except for the water(2h)–extractable HA. In addition, all the FA and HA fractions except for water(2h)–extractable HA were highly (P < 0.01) and linearly correlated to CO2 evolution, but multiple regression showed that NaOH(24h)–extractable OC was insignificant for CO2 evolution. The relatively high slope of NaOH(2h)–extractable FA versus CO2 evolution suggests that this fraction may contribute the most to compost CO2 evolution. The water(2h)– and/or NaOH(2h)–extractable FA tests are recommended for measuring compost stability because of their high correlation with CO2 evolution. This estimation can be obtained through a simple photometric method covering a wide range of carbon concentrations up to 4000 mg L−1

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Copyright © 2002. American Society of Agronomy, Crop Science Society of America, Soil Science SocietyPublished in J. Environ. Qual.31:1323–1328.