scholarly journals Effects of Prescribed Fires on Young Valley Oak Trees at a Research Restoration Site in the Central Valley of California

2011 ◽  
Vol 19 (1) ◽  
pp. 118-125 ◽  
Author(s):  
Katherine A. Holmes ◽  
Kari E. Veblen ◽  
Alison M. Berry ◽  
Truman P. Young
1992 ◽  
Vol 10 (4) ◽  
pp. 242-244
Author(s):  
Ed Perry ◽  
Gary W. Hickman

Abstract Growth of Valley Oak (Quercus lobata Neé) trees was not improved by slow-release or soluble fertilizers applied at planting time, nor by a single application of soluble fertilizer one year after planting. The native soil, with nutrient levels typical of newly developed residential and park areas in the region, provided adequate nutrition for good tree growth over the term of the 3-year study.


Plant Ecology ◽  
2005 ◽  
Vol 176 (2) ◽  
pp. 157-164 ◽  
Author(s):  
Wendy B. Trowbridge ◽  
Sara Kalmanovitz ◽  
Mark W. Schwartz

1999 ◽  
Vol 29 (2) ◽  
pp. 166-171 ◽  
Author(s):  
Kevin T Smith ◽  
Elaine Kennedy Sutherland

Fire scars result from the death of the vascular cambium resulting from excessive heating, which exposes sapwood to infection and initiates the wood decay process. In southeastern Ohio, prescribed fires in April 1995 and 1997 scarred Quercus prinus L. and Q. velutina Lam. Low-intensity fires scorched bark and produced scars, primarily on the downslope side of the stem. Eighteen scorched trees (4-23 cm at DBH) were dissected in November 1997, 14 of which had fire scars. The vascular cambium beneath natural bark fissures was most vulnerable to injury. No charred or scorched wood was associated with scars of trees exposed to single fires; wood exposed by scars from the 1995 fire was charred by the 1997 fire. Consistent with the compartmentalization process, discoloration and whiterot occurred within compartment boundaries of wood present at the time of wounding. Scars from the prescribed fires were consistent in size and shape with scars in nearby oak trees previously hypothesized to have been burned prior to 1950.


Author(s):  
Ricardo Sánchez-Murillo

This study presents a hydrogeochemical analysis of spring responses (2013-2017) in the tropical mountainous region of the Central Valley of Costa Rica. The isotopic distribution of δ18O and δ2H in rainfall resulted in a highly significant meteoric water line: δ2H = 7.93×δ18O + 10.37 (r2=0.97). Rainfall isotope composition exhibited a strong dependent seasonality. The isotopic variation (δ18O) of two springs within the Barva aquifer was simulated using the FlowPC program to determine mean transit times (MTTs). Exponential-piston and dispersion distribution functions provided the best-fit to the observed isotopic composition at Flores and Sacramento springs, respectively. MTTs corresponded to 1.23±0.03 (Sacramento) and 1.42±0.04 (Flores) years. The greater MTT was represented by a homogeneous geochemical composition at Flores, whereas the smaller MTT at Sacramento is reflected in a more variable geochemical response. The results may be used to enhance modelling efforts in central Costa Rica, whereby scarcity of long-term data limits water resources management plans.


2019 ◽  
Vol 53 (4) ◽  
pp. 265-268
Author(s):  
M. Mirab-balou

Abstract Liophloeothrips baharae sp. n. is described based on the holotype female collected on dead branches under oak trees in Zagros forests from Ilam province, western Iran. It is related to L. reperticus Ananthakrishnan and Muraleedharan, 1974 from India.


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