| View Larger Image | A quantification of short-term macroaggregate dynamics: influences of wheat residue input and texture [An article from: Soil Biology and Biochemistry] | Digitalby S. De Gryze (Author), J. Six (Author), C. Brits (Author), R. Merckx (Author)
| List Price: | $10.95 | | | Available: | Available for download now |
| | Binding: | Digital | | Publisher: | Elsevier | | Publication Date: | January 01, 2005 |
|
EDITORIAL REVIEWS |
Product Description
This digital document is a journal article from Soil Biology and Biochemistry, published by Elsevier in 2005. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.Description: Soil structure and soil aggregation play an important role in an array of processes such as soil erodibility, organic matter protection and soil fertility. Modeling attempts of these processes would benefit substantially from including soil structural parameters such as soil aggregation. However, quantitative data on soil structural dynamics is lacking. Therefore, we conducted short-term (3 weeks) incubations to acquire necessary soil structural parameters for modeling purposes. Prior to incubation, all structures >53@mm were destroyed from three soils with varying texture but under similar management. Five different amounts of wheat residue, ranging from 0 to 3wt%, were added to each of these soils. After 3 weeks, samples were analyzed for large water-stable macroaggregates (>2000@mm) using a wet sieving method and for fungal growth using epifluorescence microscopy. Aggregate formation increased linearly with increasing amounts of residue at a rate of 12.0+/-1.24g aggregates g^-^1 residue added. We found no differences in aggregate formation among the three soils, even though the equilibrium level of macroaggregates differed in the field. While amounts of water-stable macroaggregates in the sandy loam and the silt loam soil corresponded well with fungal lengths, this was not the case for the silty clay loam soil. This suggests that fungi are less important in aggregate formation in more clayey soils. Cumulative respiration correlated well (r=0.89-0.91) with water-stable macroaggregates for all three soils. A model assuming an aggregate formation rate proportional to the respiration rate was very successful in fitting the measured aggregate amounts. This model predicted about 65% of the changes in aggregation when different amounts were added, and about 85% of the changes in aggregation over time. This model yielded a macroaggregate turnover time of 40-60 days. The quantitative results presented here can directly be incorporated into models describing and predicting soil aggregate dynamics, as a determining factor for physical protection of organic matter within a soil. |
|
![A quantification of short-term macroaggregate dynamics: influences of wheat residue input and texture [An article from: Soil Biology and Biochemistry]](http://ecx.images-amazon.com/images/I/51FQM3CAMYL._SL160_.jpg)
