Vertical Dynamics of Soil Enzyme Activities and Active Organic Carbon in a Freshwater Marsh in Sanjiang Plain, Northeast China

Article Preview

Abstract:

To understand the influence of vertical dynamics of soil enzyme activities on the active carbon pool in Calamagrostis angustifolia wetland, the vertical distribution in 0-30cm depth of soil cellulase and amylase activities and active organic carbon fractions (microbial biomass carbon /MBC, easily oxidizable carbon/EOC) were measured and the relationship between soil enzyme activities and active organic carbon were analyzed. The results show that the enzyme activities and EOC and MBC contents in topsoil are the greatest. The soil cellulase and amylase activities and EOC and MBC contents show descending trends from surface layer to 30cm. The soil enzyme activities are significantly positive related to EOC and MBC contents. Therefore, with the increase of soil depth, the activities of cellulase and amylase obviously affect the soil active carbon pool. Furthermore, the cellulase activity of marsh soil has the strongest influence on soil active carbon pool.

You might also be interested in these eBooks

Info:

Periodical:

Advanced Materials Research (Volumes 998-999)

Pages:

1504-1507

Citation:

Online since:

July 2014

Authors:

Export:

Price:

Permissions CCC:

Permissions PLS:

Сopyright:

© 2014 Trans Tech Publications Ltd. All Rights Reserved

Share:

Citation:

* - Corresponding Author

[1] S. Mitra, R. Wassmann, P.L.G. Vlek. An appraisal of global wetland area and its organic carbon stock. Current Science, 88 (1), 25-35. ( 2005).

Google Scholar

[2] S.S. An, F.L. Zheng, F. Zhang, S. Van Pelt, U. Hamer, F. Makeschin. Soil quality degradation processes along a deforestation chronosequence in the Ziwuling area, China. Catena, 75, 248-256. (2008).

DOI: 10.1016/j.catena.2008.07.003

Google Scholar

[3] C. Freeman, G. Liska, N.J. Ostle, S.E. Jones, M.A. Lock, S. Hughes, B. Reynolds, J. Hudson. Enzymes and biogeochemical cycling in wetlands during a simulated drought. Biogeochemistry 39: 177–187 (1997).

DOI: 10.1023/a:1005872015085

Google Scholar

[4] D.C. Coleman, C.P.P. Reid, C. Cole. Biological strategies of nutrient cycling in soil systems. Adwances in Ecological Research, 13: 1–55. ( 1983).

DOI: 10.1016/s0065-2504(08)60107-5

Google Scholar

[5] M.M. Wander, S.J. Traina, B.R. Stinner, et al. The effects of organic and conventional management on biologically active soil organic matter fractions. Soil Sci Soc Am J, 58: l130 –l139. ( 1994).

DOI: 10.2136/sssaj1994.03615995005800040018x

Google Scholar

[6] K.Y. Chan, A. Bowman, A. Oates. Oxidizible organic carbon fractions and soil quality changes in an oxic paleustalf under different pasture leys. Soil Science 166: 61–67. (2001).

DOI: 10.1097/00010694-200101000-00009

Google Scholar

[7] Songyin Guan. Soil Enzymology and Research Method. Agricultural Press, Beijing, 1986. In Chinese.

Google Scholar

[8] J. Wu, R.G. Joergensen, B. Pommerening, R. Chaussod, P.C. Brookes. Measurement of soil microbial biomass C by fumigation-extraction -an automated procedure. Soil Biology and Biochemistry 22, 1167-1169. (1990).

DOI: 10.1016/0038-0717(90)90046-3

Google Scholar

[9] G.J. Blair, R.D.B. Lefroy, L. Lise. Soil carbon fractions based on their degree of oxidation, and the evelopment of a carbon management index for agricultural systems. Australian Journal of Agricultural Research 46: 1459–1466. (1995).

DOI: 10.1071/ar9951459

Google Scholar

[10] B.C. Liang, A.E. Mackenzie, M. Schnitzer, et a1. Management—induced change in labile soil organic matter under continuous corn in eastern Canadian soils. Biol. Fertil. Soils, 26: 88–94. (1998).

DOI: 10.1007/s003740050348

Google Scholar