4.2 Article

Using cultivated organic soil depth to form soil conservation management zones

Journal

CANADIAN JOURNAL OF SOIL SCIENCE
Volume 102, Issue 3, Pages 633-650

Publisher

CANADIAN SCIENCE PUBLISHING
DOI: 10.1139/CJSS-2021-0148633

Keywords

Organic soils; maximum peat thickness; soil conservation; soil degradation; management zones

Categories

Funding

  1. Canadian Graduate Scholarship program by the Natural Sciences and Engineering Research Council of Canada (NSERC)
  2. Master's Scholarship program (B1X) by the Fonds de recherche du Quebec-Nature et technologies
  3. NSERC [IRCPJ 411630-17]
  4. Delfland Inc.
  5. Productions Maraicheres Breizh Inc.
  6. La Production Barry Inc.
  7. Les Fermes R.R. et Fils Inc.
  8. R. Pinsonneault et Fils Ltee, Patate Isabelle Inc.
  9. Les Fermes du Soleil Inc.
  10. Les Jardins A. Guerin et Fils Inc.
  11. Le Potagers Riendeau Inc.
  12. Vert Nature Inc.
  13. Fermes Hotte et Van Winden Inc.
  14. Production Horticole Van Winden
  15. Maraichers J.P.L. Guerin and Fils

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This study focused on the cultivated organic soils in Montreal's southwest plain and characterized their physical, chemical, and pedological properties. The maximum peat thickness (MPT) was used as a proxy for soil degradation, and it was found to be moderately related to soil degradation. By dividing the study area into different management zones based on MPT thresholds, spatial differences in soil degradation were observed, highlighting the need for precision agriculture techniques for soil conservation interventions.
Cultivated Organic soils in Montreal's southwest plain are the most productive soils in the province of Quebec. After their initial drainage to enable farming, Organic soils are susceptible to many forms of degradation and soil loss. In this study, we characterized the physical, chemical, and pedological properties of 114 sites from five peatlands to form soil conservation management zones. We attempted to use the maximum peat thickness (MPT) as a soil degradation proxy. The MPT can be defined as the thickness of the layer of peat until coprogenous or mineral materials are reached. The latter are undesired growing media and are not considered in MPT calculation. A series of multivariate analysis of variance indicated that MPT was moderately related to soil degradation (optimal model's Pillai's trace = 0.495). Three soil degradation groups were defined, separated by two MPT thresholds: 60 and 100 cm. When looking at 17 different depth-property combinations, shallower sites (MPT < 60 cm) showed signs of soil degradation significantly higher than sites with an MPT above 60 cm. The second threshold was proposed for practical purposes. Then, these thresholds were used to separate the study area into spatially distinct management zones. Important spatial contrasts were found. This supports the theory that precision agriculture techniques are needed to target fields to optimize soil conservation interventions. The relationship between the MPT and soil degradation should be further explored to account for other degradation factors, and to better identify degraded soils and soils at risk.

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