101-2 Rootzone pH and Penn A-4 Creeping Bentgrass Root Growth.

See more from this Division: C05 Turfgrass Science
See more from this Session: Establishment, Thatch, Soil and Water Management in Turfgrass Graduate Student Competition
Monday, October 22, 2012: 8:20 AM
Millennium Hotel, Grand Ballroom A, Second Floor
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Derek T. Pruyne and Maxim J. Schlossberg, Center for Turfgrass Science, Penn State University, University Park, PA
Rootzone pH highly influences nutrient availability and root growth during both establishment and maintenance of creeping bentgrass (Agrostis stolonifera L. ‘Penn A-4’) putting greens (PGs). While the optimal pH range for creeping bentgrass is generally considered to be 5.5–6.5, PG sand rootzones across the Mid-Atlantic and Midwest regions frequently contain calcite and are buffered to higher pH values. Further alkalinization, via topdressing sand and/or irrigation water inputs, offsets natural acidification processes at the PG surface. Meanwhile, our understanding of how supraoptimal rootzone pH influences Penn A-4 root growth remains limited. A greenhouse study evaluated Penn A-4 root growth, viability, and distribution over an array of rootzone pH levels (5-7.5), yet otherwise receiving ample maintenance fertilization. Furthermore, rootzone samples collected from PG field studies conducted in 2007, 2011, and 2012 were analyzed for soil pH (1:1 DI-H2O), root length density, specific root length, and specific fork number (forks/g). A ‘metadata’ analysis approach, using these and other published findings, generates a more specific soil pH range for optimal root growth of Penn A-4 creeping bentgrass maintained as PGs.
See more from this Division: C05 Turfgrass Science
See more from this Session: Establishment, Thatch, Soil and Water Management in Turfgrass Graduate Student Competition