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The Role of Nutrients in Building Soil Carbon
Liming and Soil Acidity
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Authors
Carpenter-Boggs, L
Carter, P
Evans, C
Huggins, D
Moore, A
Shiwakoti, S
Sullivan, D
Van Vleet, S
Wieme, R
Topics
Liming and Soil Acidity
Type
Oral
Year
2021
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Filter results3 paper(s) found.

1. Evaluation of Lime Requirement Estimation Methods for Oregon Agricultural Soils

Soil testing labs in the Pacific Northwest are considering non-hazardous alternatives to the Shoemaker-McLean-Pratt (SMP) buffer method for lime requirement estimation (LRE). While alternative LRE methods have been adopted in other parts of the U.S., they have not been evaluated for Oregon soils.  The goal of this study was to evaluate several LRE methods for agricultural soils from western and eastern Oregon, applying the lime incubation method for actual lime requirement. Twenty-four a... C. Evans, A. Moore, D. Sullivan

2. Effects of Lime and Micronutrient Amendments for Acidic Soils of the Inland Pacific Northwest

The soil pH of agricultural land in the inland Pacific Northwest has dropped precipitously from native soil levels of near 7.0 pH. Changes that were becoming evident in the 1980’s have reached critical levels, leaving tens of thousands of acres of previous prairie soil at pH under 5.0 and unable to grow an increasing number of aluminum-sensitive crops. Some farmers in the region are beginning to use lime application to neutralize soil acidity. However, pH changes and liming can als... R. Wieme, L. Carpenter-boggs, P. Carter, S. Van vleet

3. Long-term Soil Profile Acidification: Obvious and Hidden Dangers

Soil acidification is occurring in the dryland farming region of the Northwest. Historically, soil acidification in the surface foot has been characterized; however, potential acidification of subsoil is unknown. We examined soil acidification for soil profiles (0 to 5 ft) at the R.J. Cook Agronomy Farm (92 ac) for 17 years following conversion from conventional tillage to continuous No-tillage (NT). Surface soil depths (0-12 in) acidified under continuous NT to below 5. Surprisingly, subsoil... D. Huggins, S. Shiwakoti