z-logo
Premium
Long‐term Dryland Crop Responses to Residual Phosphorus Fertilizer
Author(s) -
Halvorson A. D.,
Black A. L.
Publication year - 1985
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj1985.03615995004900040028x
Subject(s) - loam , fertilizer , agronomy , crop , phosphorus , human fertilization , soil test , soil water , randomized block design , environmental science , zoology , mathematics , chemistry , biology , soil science , organic chemistry
Little information is available on the long‐term effects of a single P fertilizer application on grain yields of crops grown on dryland soils deficient in plant‐available P. Therefore, duplicate plots were established in 1967 and 1968 on a Williams loam (fine‐loamy mixed, Typic Argiborolls) with a NaHCO 3 −extractable P of 6 mg P/kg soil. A split‐plot, randomized complete block design was used with three levels of available N (generally 0, 45, and 90 kg N/ha each crop year) as main plots and a one time application of P fertilizer at rates of 0, 22, 45, 90, and 180 kg P/ha as subplots. During the first crop year, application of 22, 45, 90, and 180 kg P/ha raised the average soil test P levels to 9, 12, 26, and 40 mg P/kg soil, respectively. Soil test P levels 16 yr after P fertilization and 10 or 11 crops harvested avg 5, 6, 7, 9, and 13 mg P/kg soil in 1983 for these same respective P treatments. Soil test P levels declined progressively with each additional crop year until the eighth crop or 13 yr after P application, at which time a new soil P equilibrium level appeared to be developing. Grain yields generally increased with increasing residual soil P level when adequate levels of N, either residual or applied, were present. However, no response to increasing residual soil P level was observed under annual cropping without adequate N. Accumulated grain yields after 10 or 11 crops were about three times greater with both N and P fertilization than with P fertilization alone. The study verifies that adequate available N is required to derive benefit from residual P fertilizer. The long‐term (16 yr) residual benefits from P fertilization suggest a method for possibly satisfying the P needs for several crop years in reduced and notillage systems, if the P is applied and incorporated before initiation of these tillage systems.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom