Effects of calcium silicate treatment on the composition of forest floor organic matter in a northern hardwood forest stand
- 291 Downloads
Calcium amendment can help improve forest sustainability in stands that have been impacted by chronic acid deposition. An important component of this improvement is the stimulation of the microbial activity that supports ecosystem nutrient cycling processes. To test the hypothesis that Ca treatment alters the structure and solubility of organic matter substrates, an important driver of microbial activity, we investigated the effect of wollastonite (CaSiO3) treatment on soil organic matter (SOM) and hot-water-extractable organic matter (HWEOM). We found a decrease in the HWEOM content of forest floor soils within 2 years of treatment with a high dosage of wollastonite (4,250 kg Ca/ha), but not at a low dosage (850 kg Ca/ha). High-dosage treatment did not reduce the biodegradability of HWEOM. Hence, a high dose of CaSiO3 appears to reduce the solubility of organic matter in the forest floor but not the bioavailability of the extracted SOM. Nuclear magnetic resonance spectroscopy revealed no significant changes in the O-alkyl C content of SOM in response to wollastonite addition, but a reduction in the O-alkyl C content of HWEOM suggests that the extractability of carbohydrate structures was reduced by added CaSiO3. Phosphorous treatment, when performed in combination with Ca, also decreased the O-alkyl C content of HWEOM, but had no effect when performed without Ca. The reduced solubility of SOM after Ca treatment may have been the result of bridging between Ca2+ and negatively charged sites on SOM, as suggested in other studies. Also, high concentrations of Si in soil solution, due to dissolution of the wollastonite, likely resulted in oversaturated conditions with respect to SiO2 or kaolinite, perhaps leading to co-precipitation of soluble organic matter. Overall, our results suggest that added Ca and/or Si may react with SOM to reduce the accessibility of labile C forms to soil microbes.
KeywordsCalcium Forest soil Hot-water extractable organic matter Nuclear magnetic resonance spectroscopy Phosphorus Soil carbon Soil organic matter
We gratefully acknowledge the United States Department of Agriculture (USDA) NRI Competitive Grants Program (award no. 2005-35107-16200) and the National Science Foundation Long-Term Ecological Research Program (Grant No. 1114804) for support of this research. Ankit Balaria held the Wen-Hsiung and Kuan-Ming Li Graduate Fellowship in the Department of Civil and Environmental Engineering at Syracuse University while conducting this research. We appreciate the help of Mary Margaret Koppers, Mario Montesdeoca, Lisa Martel, Colin Fuss, and David Kiemle. This is a contribution to the Hubbard Brook Ecosystem Study. The Hubbard Brook Experimental Forest is administered by the USDA Forest Service Northern Research Station, Newtown Square, PA.
- Baath E, Berg B, Lohm U, Lundgren B, Lundkvist H, Rosswall T, Soderstrom B, Wiren A (1980) Effects of experimental acidification and liming on soil organisms and decomposition in a Scots pine forest. Pedobiologia 28:85–100Google Scholar
- Bohlen PJ, Groffman PG, Driscoll CT, Fahey TJ, Siccama TG (2001) Plant–soil–microbial interactions in a northern hardwood forest. Ecology 82:965–978Google Scholar
- Filep T, Szili-Kovács T (2010) Effect of liming on microbial biomass carbon of acidic arenosols in pot experiments. Plant Soil Environ 56:268–273Google Scholar
- Griffin EM (1985) A comparison of the roles of bacteria and fungi. In: Leadbetter ER, Poindexter JS (eds) Bacteria in Nature, vol. 1. Bacterial activities in perspective. Plenum Press, New York, pp 221–255Google Scholar
- Persson T, Lundkvist H, Wiren A, Hyvonen R, Wessen B (1989) Effects of acidification and liming on carbon and nitrogen mineralization and soil organisms in mor humus. Water Air Soil Pollut 45:77–96Google Scholar
- Speir TW, Ross DJ (1978) Soil phosphatase and sulphatase. In: Burns RG (ed) Soil Enzymes. Academic Press, London, pp 197–250Google Scholar