Controls on Forest
Soil Organic Matter Development and Dynamics: Chronic Litter Manipulation as a
Potential International LTER Activity.
Nadelhoffer, Knute
The Ecosystems Center,
Marine Biological Laboratory, Woods Hole, MA 02543, USA
Abstract
Organic
matter (or humus) content strongly influences key soil properties such as
moisture holding capacity, aeration, and cation retention in terrestrial
ecosystems. It also constitutes large reservoirs of nutrients and reduced
carbon that fuel microbial processes and support complex communities of soil
and forest floor organisms.
Because nutrient cycles are relatively closed in most forests, trees and
understory plants depend mainly on the nutrients released from decomposing
organic matter to meet their nutritional requirements. As such, the amount and the quality of
soil organic matter greatly influence primary production and ecosystem
biogeochemical cycles.
Despite
the critical roles of soil organic matter, the degree to which above- and
belowground plant inputs influence its formation and dynamics is not well
understood. To address this gap,
my collaborators and I established a long-term study of controls on soil
organic matter formation: the DIRT (Detritus Input Removal and Transfer)
project. The goal of the DIRT project is to assess how rates and sources of plant litter inputs control the accumulation
and dynamics of organic matter and nutrients in forest soils over decadal time scales.
DIRT
treatments consist of chronically altering above- and belowground plant inputs
to permanent plots in a mid-successional oak-maple-birch forest at Harvard
Forest in the northeastern US.
Treatment
|
Manipulation
|
|
CONTROL |
(normal litter inputs) |
|
NO
LITTER |
(aboveground litter excluded from plots) |
|
DOUBLE
LITTER |
(twice aboveground litter inputs) |
|
NO
ROOTS |
(roots excluded from plots by lined trenches) |
|
NO
INPUTS |
(no aboveground litter and no roots) |
|
O/A‑LESS |
(organic and A horizons replaced with B horizon soil,
normal inputs thereafter) |
The
DIRT project has the potential to become a long-term, intersite
experiment. To that end we have
forged linkagess with similar and experiments at sites in a nutrient-rich maple
forest in Pennsylvania (Allegheny College Bousson Environmental Research
Reserve) and an old-growth forest in Oregon (H. J. Andrews Experimental Forest
USFS). We hope to develop
additional linkages to similar experiments located across climate and soil
texture gradients. This will allow
an assessment of the importance of physical as well as biological factors in
controlling soil organic matter accumulation. At the international LTER meeting to be held in Korea in
1999, I will present selected results from the first decade of DIRT
manipulations at the Harvard Forest site to illustrate how chronic alterations
of leaf and root inputs to soils can provide valuable information about short-
and long-term processes in ecosystems.