Abstract

AbstractMany agricultural soils of the northern Great Plains have excess CaCO3 or CaSO4 and pH levels above 7.8, thereby having high fixation capacity for applied P and resultant poor predictability of crop responses to applied P fertilizer. In addition, initial and residual effects of applied fertilizer P on soil test P values are not well understood. A greenhouse study was conducted with Sordan 79 (sordan), an intraspecific [Sorghum bicolor (L.) Moench] sorghum‐sudangrass hybrid [syn. S. bicolor‐S. sudanense (Piper) Stapf], on three soils with different textures, cation exchange capacities, and CaCO3 contents to determine sordan response to P fertilizer applied to calcareous soils. Soil test P (bicarbonate‐extractable) was adjusted to five initial levels, ranging from 2 to 60 μg P g−1 soil. Fertilizer P was then applied at five levels, ranging from 0 to 40 mg P kg−1 soil. Three successive harvests of the test crop were completed and measurements of dry matter were made. Response surfaces and regression models were developed, describing the relationships among sordan yield, P uptake by the crop, total P applied as fertilizer, and resultant soil test P values. Sordan response to P fertilizer was linear at soil test values of <30 μg P g−1 soil, but the response was curvilinear above soil test values of 30 μg P g−1 soil. However, soils with lower soil test levels did not yield as much, even at the highest P rates, as those soils testing above 30 μg P g−1 soil and with no additional P added. The preplant soil test P concentrations as well as the residual (postexperiment) bicarbonate‐extractable P soil test concentrations increased with increasing rate of fertilizer P. Results of this study suggest advantages of fertilizer strategies that elevate the bicarbonate‐extractable P soil test values of agricultural soils having excess CaCO3 and pH values above 7.8. Only maintenance applications of fertilizer P appear to be necessary when soil test P concentrations are at or above 30 μg P g−1 of soil and these same soils have relatively high CaCO3 or CaSO4 concentrations.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.