91014
Dry Matter and Potassium Accumulation and Partitioning in Three Soybean Genotypes.

See more from this Division: Submissions
See more from this Session: Graduate Student Oral Competiton – Soils
Monday, February 2, 2015: 1:15 PM
Westin Peachtree Plaza, Chastain F
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Md. Rasel Parvej1, Nathan A. Slaton1, Trenton L. Roberts2, Russell E. DeLong2, Randy J. Dempsey2 and Matthew S. Fryer2, (1)Crop, Soil, and Environmental Sciences, University of Arkansas, Fayetteville, AR
(2)University of Arkansas, Fayetteville, AR
Understanding the K uptake pattern during the growing season is required to develop sound fertilization programs. We measured season-long aboveground dry matter and K accumulation and allocation in representative determinate [maturity group (MG) 5.3 (2012) or 5.5 (2013)] and indeterminate (MG 3.9 and 4.7) soybean [Glycine max (L.) Merr.] cultivars in 2012 and 2013. Whole-plants and recently matured trifoliolate-leaves were collected 8-10 times between V5 and maturity. Each parameter was statistically analyzed by year due to differences in planting date. In 2012, the maximum dry matter accumulation among cultivars was similar (10.3-11.6 Mg ha-1). In 2013, aboveground dry matter was similar for both indeterminate cultivars (7.5-8.0 Mg ha-1) but less than the determinate cultivar (9.7 Mg ha-1). Dry matter accumulation peaked at R6.0-6.5, 96-102 (2012) and 82-96 (2013) days after emergence (DAE). The predicted maximum crop growth rate occurred at R4-5 stage [180-197 (2012) and 144-167 (2013) kg dry matter ha-1 d-1]. Each year, the maximum aboveground K uptake was similar among cultivars totaling 118-148 (2012) and 125-132 (2013) kg K ha-1 and peaking at R5.5-6.0, 93-111 (2012) and 74-94 (2013) DAE. The predicted maximum K uptake rate occurred at R3-4 stage [2.01-2.27 (2012) and 1.77-2.39 (2013) kg K ha-1 d-1]. Before leaf senescence (R7), seed comprised 40-51% of the aboveground dry matter (7.2-10.7 Mg ha-1) and 49-69% of the aboveground K content (114-138 kg K ha-1). In 2012, trifoliolate-leaf K concentration for all cultivars peaked at R2 (14.2-16.3 g K kg-1) and declined linearly at a rate of 0.16 g K kg-1 d-1 until R7. In 2013, trifoliolate-leaf K concentration peaked at R1 (19.8-20.6 g K kg-1) and declined linearly, but differently among cultivars (0.06-0.21 g K kg-1 d-1). This information may aid in developing critical trifoliolate-leaf K concentrations beyond the R1-2 stage for diagnosis of K deficiency.
See more from this Division: Submissions
See more from this Session: Graduate Student Oral Competiton – Soils