Recipient Organization
CORNELL UNIVERSITY
(N/A)
ITHACA,NY 14853
Performing Department
Natural Resources
Non Technical Summary
In 2012, we initiated a field study to quantify sources of forest soil organic carbon using isotope-labeled plant detritus. Forest ecosystems play a major role in the global carbon cycle storing carbon in both live biomass and in soil organic matter. The effects of forest harvest on soil C sequestration are difficult to quantify because of the large, slowly changing pool size and high spatial variation; hence, the response of soil C to forest management activity is poorly constrained, and the process of soil organic formation is incompletely understood. This project utilizes isotope-labeled leaf litter, coarse woody debris, fine roots and woody roots, to investigate the process of soil organic matter formation. This research will enable more accurate predictions of the response of soil C pools to environmental changes and forest management activities, essential for evaluating this important sink in the global carbon budget. Such knowledge is essential for decision making in the realm of local, regional and global greenhouse gas management. The experiments are in place at two sites and results from the first-year collection (2013) for fine roots indicate that we will be able to quantify C sequestration in various soil aggregate pools in five different regional soil types with high accuracy and precision. Collection of the woody substrate samples are planned for years 3-6 (2015-2018).
Animal Health Component
(N/A)
Research Effort Categories
Basic
100%
Applied
(N/A)
Developmental
(N/A)
Goals / Objectives
The goal of the proposed research is to increase understanding of the process of stabilization of detrital C in forest soil. 1. To quantify the transformation of C in woody debris into underlying soil; the pools of soil carbon to which it contributes; and the effect of different classes of wood decay fungi (white vs. brown rot) in contributing to sequestration of woody debris carbon in soil. 2. To quantify stabilization of C from fine root detritus in different soil aggregate pools in comparison with leaf litter. 3. To quantify stabilization of C in woody root detritus in soil aggregate pools. 4. To inform policy makers of the implications of the research for long-term effects of intensified forest harvest on soil C sequestration.
Project Methods
We are utilizing plant tissues highly-enriched in 13C, including leaf litter, fine roots, woody roots and stem wood, to trace C into soil pools. The field study was initiated in 2012 and consists of three components, addressing the first three objectives. Study 1. The experimental design includes three treatments in terms of decay fungi: white-rot (inoculated), brown-rot (inoculated) and naturally occurring taxa (not inoculated). We plan to collect randomly-selected samples in 2015 (3 yr), 2016 (4 yr) and 2017 (5 yr). Enrichment of 13C will be quantified in each of six soil pools, including different soil aggregate components. Study 2. We inoculated highly 13C-enriched very fine (< 1mm) and fine (1-2 mm) in soil cores containing soil from five different regional soil horizons, including inceptisols, alfisols and spodosols. We have completed two collections from this study (2013 and 2014) and collections are planned for year 3 and 4. Again, enrichment of several soil fractions will be quantified. Study 3. We are tracing 13C from the woody roots of labeled trees (seven labeling chambers) into soil C pools. In 2012 we quantified 13C pools (one year after tree stems were harvested) to initiate this study. Soil pits will be excavated in year 3-6 (2015-2018), and 13C enrichment in various soil pools will be measured.