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Atlantic Forestry Centre
Science > Ecology and EcosystemsSoil is the basis of life > Soil Science

Soil Science
Dr. M.K. Mahendrappa

Soil is the Basis of Life

Dr. Mahendrappa's research focuses on understanding the nutrient cycling processes in the forest ecosystems. Using this basic information he is seeking means to establish relationships between forest harvesting options and soil productivity, specifically:

  • consequences of removing varying intensities of forest biomass from harvested areas
  • alternative harvesting options
  • impacts on soil chemistry and soil productivity
Dr. Mahendrappa employs a special tool, called a lysimeter, to collect soil solution samples without disturbing the soil. Various nutrients/elements are measured in the soil solution to evaluate the potential impacts of different types of harvesting regimes.
  • Lysimeters collect leachate from the soil, which can then be analyzed for nutrient content.
  • Lysimeters consist of a glass housing, 6 cm in diameter, fitted with a fritted glass disk fused in place. The fine pores in the fritted disks allow only soil solutions through and keep soil particles out. The lysimeter connected to a sample collection bottle, to a vacuum generating system is called a lysimeter system.
  • By analyzing the concentrations of nutrients in leachates collected in the forests subjected to various harvesting regimes, we can evaluate the potential effects of harvesting and site preparation methods on soil quality.
Soil is the basis of life on earth. The soil is a living entity, containing millions of organisms essential to the cycling of nutrients. The soil acts as a filter protecting lakes and streams.
  • Results of studies indicate that a high proportion of inherent nutrient reserves is removed from forests in whole-tree harvesting, compared to conventional (stem only) harvesting.
  • Nutrient depletion of the soil leads to reduced soil fertility.
  • As a result of whole-tree harvesting, the surface soil temperature increases, which in turn causes faster decomposition of soil organtic matter (OM)- the storage of all nutrients.
  • Increased incidence of solar radiation results in faster biochemical reactions that ultimately lead to (OM) decomposition and site degradation.
  • Degraded (acidified) soils are incapable of sustaining healthy tree growth during subsequent rotations.
Atlantic Forestry Centre
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