USDA.gov
Agspace Masthead
  HomeAbout AgSpaceNewsCurrent ProjectsagricolaHelpContact Us
 Search National Agricultural Library
 
advanced search
search tips
browse by subject
Submit to AgSpace
usda
Browse by subject
updates
profile
 
Please use this persistent URL to cite or link to this item:
http://hdl.handle.net/10113/10732 ◀ bookmark this

Files in This Item:

File SizeFormat
IND44014685.pdf653KbAdobe PDFView/Open
Title: Influence of Thinning Loblolly Pine ( Pinus taeda L.) on Hydraulic Properties of an Organic Soil.
Authors: Grace, J.M. III
Skaggs, R.W.
Cassel, D.K.
USDA, FS
Source: Transactions of the ASABE. 2007 Mar-Apr, v. 50, no. 2, p. 517-522.
NALT Subjects: Pinus taeda
forest plantations
forest thinning
soil compaction
drainage
forest soils
organic soils
soil physical properties
saturated hydraulic conductivity
bulk density
soil water content
porosity
North Carolina
Other Subjects: drained volume
drainable porosity
Issue Date: Mar-2007
Abstract: The impact of forest operations on soil properties has been a concern in forest management over the past 30 years. The objective of this study was to evaluate the impact of forest thinning operations on soil hydraulic properties of a shallow organic (Belhaven series) soil in the Tidewater region of North Carolina. Soil physical properties were evaluated in a nested design by collecting soil cores from an unthinned control and following a 40 ha fifth-row thinning with selection performed on a 14-year-old loblolly pine plantation in April 2001. Thinning decreased saturated hydraulic conductivity and drained volumes for a given water table depth; however, changes in bulk density were not detected. Saturated hydraulic conductivity determined by the constant head method before thinning was 100 cm h(-1). Thinning resulted in a 3-fold decrease (from 100 to 32 cm h(-1)) in saturated hydraulic conductivity. The thinned watershed had less drainage at low pressures and greater retained water contents under increased soil water tensions in comparison with the control. Drained volume on the thinned watershed for a water table depth of 200 cm under drained to equilibrium conditions was reduced by 60% in comparison to drained volume for the control watershed. The reductions in k(sat), drained volumes, and drainable porosity will likely result in shallower water tables and increased runoff for the thinned watershed.
URI: http://hdl.handle.net/10113/10732
Appears in Collections:USDA Research and Information

Files in This Item:

File SizeFormat
IND44014685.pdf653KbAdobe PDFView/Open

--------- --------- ----------------


Powered by DSpace

 DDR Home | AgSpace Home | NAL Home | USDA | ARS | Science.gov | GPO Access | Policies and Links | FOIA | NAL Thesaurus
Accessibility Statement | Privacy Policy | Non-Discrimination Statement | Information Quality | USA.gov | White House