Long‐term dairy manure amendment promotes legacy phosphorus buildup and mobility in calcareous soils

Author:

Hu Ruifang1,Leytem April B.2ORCID,Moore Amber D.3ORCID,Strawn Daniel G.1ORCID

Affiliation:

1. Department of Soil and Water Systems University of Idaho Moscow Idaho USA

2. Northwest Irrigation and Soils Research Lab USDA‐ARS Kimberly Idaho USA

3. Department of Crop and Soil Science Oregon State University Corvallis Oregon USA

Abstract

AbstractContinuous application of dairy manure to soils can lead to excessive phosphorus (P) accumulation (legacy P), which requires understanding for managing nutrient availability and leaching. This study was conducted in Kimberly, ID, where dairy manure or conventional fertilizer was applied to calcareous soil plots under continuous crop rotations for 8 years (2013–2020), followed by 2 years with no amendment. To understand legacy P behavior in the soils, total P, organic/inorganic P, and plant‐available Olsen bicarbonate P and Truog extraction measurements were made from surface and subsurface samples. Additionally, P in soluble and less soluble calcium phosphate (Ca‐P) minerals was estimated using selective extractions, and P desorption was measured in a flow‐through reactor. Manure amendments resulted in increased total soil P and plant‐available P, particularly in the initial 5 years. In the 0‐ to 30‐cm depth, 54%–65% of the soil P added from manure amendments was readily soluble by the Truog P test. Phosphorus released from the 2022 manure‐amended soil in the desorption experiments was about five times greater than the fertilizer‐amended soil, suggesting high leaching potential. After 8 years of manure amendment, subsurface Olsen‐P levels exceeded the 40 mg kg−1 management threshold, suggesting P adsorption potential of the surface had become saturated, allowing for P leaching. In the manure‐amended surface soils, calcium phosphate minerals increased compared to the controls. Even after 2 years without manure amendment, soluble Ca‐P mineral phases persisted in the soils, which can be a long‐term source of P leaching.

Funder

National Institute of Food and Agriculture

Publisher

Wiley

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