scholarly journals Long-term tree productivity of a South Carolina coastal plain forest across a hydrology gradient

2011 ◽  
Vol 4 (1-2) ◽  
pp. 67-76 ◽  
Author(s):  
W. H. Conner ◽  
B. Song ◽  
T. M. Williams ◽  
J. T. Vernon
Keyword(s):  
2012 ◽  
Vol 76 (5) ◽  
pp. 1036-1046 ◽  
Author(s):  
Cathryn H. Greenberg ◽  
Douglas J. Levey ◽  
Charles Kwit ◽  
John P. Mccarty ◽  
Scott F. Pearson ◽  
...  

1994 ◽  
Vol 72 (11) ◽  
pp. 1945-1950 ◽  
Author(s):  
David G. Krementz ◽  
Grey W. Pendleton

The long-term decline of the American woodcock (Scolopax minor) population led us to investigate diurnal habitat use with radiotelemetry on the wintering grounds. Sites included the coastal plain of Georgia (1989–1991), South Carolina (1988–1989), and Virginia (1991–1992). Habitat use was not explained by age, sex, or date during the winter, but individuals used habitat differently (P < 0.05). Only shrubland was preferred at all sites in all years. Pine plantations of various ages were used according to availability, but usually less often than expected, while bottomland hardwoods and pine–hardwoods were used more often than expected.


2020 ◽  
Author(s):  
Jessica Kasten ◽  
Elizabeth Lewis ◽  
Sari Lelchook ◽  
Lynn Feinberg ◽  
Edem Hado

2015 ◽  
Vol 86 (4) ◽  
pp. 337-344 ◽  
Author(s):  
Mark Vukovich ◽  
Kelsey L. Turner ◽  
Tracy E. Grazia ◽  
Thomas Mims ◽  
James C. Beasley ◽  
...  

1987 ◽  
Vol 77 (6) ◽  
pp. 2143-2151
Author(s):  
Susan Rhea

Abstract Phase conversions from P to SV and from SV to P occur at a high impedance boundary near the surface in Charleston, South Carolina. Four arrivals (P, converted P, converted S, and S) are observed on three-component records of earthquakes in this area. Using arrival-time differences between paired arrivals of direct and converted phases, a shallow surface layer Vp/Vs ratio of 2.9 was determined. Applying the Wadati method to travel times derived at the base of the surface layer yields a Vp/Vs ratio in deeper layers of 1.73. Relocating earthquakes using this more appropriate velocity structure for direct and converted shear waves alters hypocentral parameters such that epicenters diverge and depths converge. It is inferred that these relocated earthquakes are not exclusively associated with a single seismogenic fault.


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