|
|
||||||||
a USDA-ARS, Sugarcane Field Station, 12990 U.S. Hwy. 441, Canal Point, FL 33438
b Everglades Research and Education Center, Univ. of Florida, 3200 East Palm Beach Road, Belle Glade, FL 33430
c USDA-ARS, North Central Soil Conservation Research Laboratory, 803 Iowa Ave., Morris, MN 56267
* Corresponding author (dmorris{at}saa.ars.usda.gov)
Organic soils in the Everglades Agricultural Area (EAA) of southern Florida, USA, are subsiding due primarily to oxidation by aerobic microorganisms. Since there are large C losses in drained Histosols, it is not certain if minimum tillage will significantly reduce soil C losses below the background levels. The objective of this experiment was to determine if increasing the surface soil disturbance through tillage significantly increases the soil organic matter oxidation potential (OP) in Histosols. Tillage treatments from lowest to highest soil disturbance consisted of (i) no-till; (ii) tine implement cultivation, one pass; (iii) tine implement cultivation, two passes; (iv) heavy harrow disking; and (v) switchplowing. Treatments were conducted on two fields (bare fallow and plant residue covered). Surface soil samples (015 cm) and all microbial measurements were taken on 0, 1, 4, 13, 28, and 42 d after tillage. The switchplow treatment had the greatest OP (14C oxidation of benzoate) and soil microbial CO2 respiration (RESP) averaged across the 42-d period compared with the other treatments. No-till tended to have the lowest OP and RESP. Other tillage treatment effects were intermediate depending on field type. Correlation analyses indicated that greater quantities of extractable N (EXN) were related to increased OP in both fields, while higher quantities of extractable C (EXC) were related to increased RESP in both fields. This research demonstrates that minimum tillage can be used on Histosols to reduce C loss and thereby reduce soil subsidence.
Abbreviations: EAA, Everglades Agricultural Area EXC, extractable organic carbon (mg C g1 soil) EXN, extractable total nitrogen (mg N kg1 soil) MBC, microbial biomass carbon (mg C g1 soil) MBN, microbial biomass nitrogen (mg N kg1 soil) OP, organic matter oxidation potential (nmol CO2 kg1 soil h1) RESP, microbial respiration (µmol CO2 m2 s1)
This article has been cited by other articles:
![]() |
R. A. Omonode, A. Gal, D. E. Stott, T. S. Abney, and T. J. Vyn Short-term Versus Continuous Chisel and No-till Effects on Soil Carbon and Nitrogen Soil Sci. Soc. Am. J., February 2, 2006; 70(2): 419 - 425. [Abstract] [Full Text] [PDF] |
||||
![]() |
R. Lal, M. Griffin, J. Apt, L. Lave, and G. Morgan Response to Comments on "Managing Soil Carbon" Science, September 10, 2004; 305(5690): 1567d - 1567d. [Full Text] [PDF] |
||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| The SCI Journals | Agronomy Journal | Crop Science | |||
| Vadose Zone Journal | Journal of Plant Registrations | ||||
| Journal of Natural Resources and Life Sciences Education |
Journal of Environmental Quality |
||||