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United States Department of Agriculture

Agricultural Research Service

Research Project: Simulationg soil organic matter dynamics of the long-term plots at CBARC using the CQESTR model

Location: Soil and Water Conservation Research

2011 Annual Report

1a. Objectives (from AD-416)
The objective of this cooperative research project is to investigate soil organic carbon dynamics in the long-term plots at CBARC in Pendleton using a process-based soil carbon (C) model, the CQESTR model. Specifically this project is conducted to: 1) determine soil organic carbon dynamics over 75 years of repeat additions or removal of carbon sources, fertilizer levels, and tillage practices; 2) predict the potential of C accretions or losses with varying crop rotation, tillage, and amendment scenarios.

1b. Approach (from AD-416)
Long-term field experiments (LTE) with repeat additions or removal of carbon sources are ideal to examine soil organic carbon (SOC) dynamics and validate soil C models. CBARC is home to the oldest experiments in the western U.S. with some of the experiments dating back to the 1931. The management and treatments of most of the experiments have changed little since their establishment. Several residue burn treatments had a minor change in 1978. Nitrogen was broadcast as (NH_4)_2SO_4 from 1931 to 1961 and as NH_4NO_3 since 1962. The spring residue burning with no N addition, fall burning with no N addition, manure application at 11.2 t/ha/yr (741 kg C and 56 kg N/ha/yr), pea vine addition at 1.12 t /ha/yr (397 kg C and 17 kg N/ha/yr), or no residue burning with 0, 45, and 90 kg N/ha have all been in place since 1967. These treatments were initiated to diminish or eliminate the detrimental effects of conventional tillage winter wheat-summer fallow system, which is the predominant cropping system in the Pacific Northwest, on SOC. Soil carbon content of these long-term plots is determined every 10 years. The collected SOC data will be used to prepare a database for these fields to elucidate the effect of repeat additions or removal of carbon sources on soil carbon accretion or loss. Soil carbon dynamics during 75 years will be determined. CQESTR, a C balance model developed by ARS scientists at the Columbia Plateau Soil Conservation Research Center (CPCRC) in Pendleton, will be used to predict SOC status at the field-scale. RUSLE files (c-factor files) for LTE plots will be prepared for use with CQESTR. Simulation runs with the CQESTR model will be performed to predict changes in SOC. Simulation results will be compared to the measured SOC. The influence of repeat additions or removal of carbon sources or different C sources on SOC will be determined. Prediction runs with the CQESTR model will be undertaken with varying crop rotation, tillage, and amendment scenarios.

3. Progress Report
This research relates to objective 1b of the parent project. Crop residues play a vital role in maintaining soil organic matter, which is not only required for preserving soil functions, but also for ensuring the sustainable long-term production of biofuel feedstock. Databases for five long-term experiments in North America (Breton, AB, Canada, Morrow, IL, Pendleton, OR, Sanborn, MO, Lethbridge, AB, Canada) were prepared. RUSLE c-factor files were established for no-till simulations under various agricultural management systems. The CQESTR model simulated soil organic carbon dynamics for conventional tillage were compared with measured data. The potential of soil organic carbon stocks maintenance for no-till with five residue removal rates scenarios were predicted. Using fertilizer alone was insufficient to overcome residue removal impact on soil organic carbon. Manure or cover-crop/intensified crop rotation under no-till were options to mitigate loss of crop residue carbon from agricultural soils. These results will have important implications for farmers, crop advisors, scientists, and policy makers interested in biofuel. This project is monitored by phone calls, electronic mail, and reports.

4. Accomplishments

Last Modified: 06/23/2017
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