Carl Mendoza

Carl Mendoza

orcid

Research Focus & Metrics

Academic Career Length

37Years (1990-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

View All Publications
26 April 2005 in Hydrological Processes
Verified
Journal Article
Closed access
PDF file
KDK. Devito
K. Devito
ICI. Creed
I. Creed
TGThian Yew Gan
Thian Yew Gan
CMCarl Mendoza
Carl Mendoza
RPR. Petrone
R. Petrone
BSB. Smerdon
B. Smerdon

1 November 2005 in Journal of Hydrology
Verified
Journal Article
Closed access
BSB.D. Smerdon
B.D. Smerdon
KDK.J. Devito
K.J. Devito
CMCarl Mendoza
Carl Mendoza

1 September 2008 in Canadian Journal of Forest Research
Verified
Journal Article
Closed access
KBKevin Bladon
Kevin Bladon
USUldis Silins
Uldis Silins
MWMichael J. Wagner
Michael J. Wagner
MSMicheal Stone
Micheal Stone
Monica EmelkoMonica Emelko
Monica Emelko
SBSarah Boon
Sarah Boon
The objective of this study was to examine initial effects of the 2003 Lost Creek wildfire (southwestern Rocky Mountains of Alberta) on concentrations and production (yield and total export) of several nitrogen (N) forms, and to explore initial recovery of these effects within the first 3 years after the fire. During the first postfire year, nitrate (NO3–), dissolved organic nitrogen (DON), and total nitrogen (TN) concentrations in severely burned watershed streams were 6.5, 4.1, and 5.3 times greater, respectively, than those in reference streams. Weaker effects were evident for concentrations of ammonium (NH4+; 1.5 times) and total particulate nitrogen (TPN; 3.0 times). A rapid decline in mean watershed concentrations and production of NO3–, DON, total dissolved nitrogen (TDN), and TN was observed from burned watersheds over the three seasons after the fire. However, elevated NO3–, TDN, and TN concentrations and production were still evident during the snowmelt freshet and following precipitation events after 3 years. Effects of the burn were strongly influenced by the regional flow regime, with the most elevated N concentrations and production occurring during higher discharge periods (snowmelt freshet and storm flows).

1 April 1994 in Water Resources Research
Verified
Journal Article
Closed access
PDF file
RSRobert A. Schincariol
Robert A. Schincariol
FSFranklin W. Schwartz
Franklin W. Schwartz
CMCarl Mendoza
Carl Mendoza

8 January 2010 in Hydrological Processes
Verified
Journal Article
Closed access
PDF file
SBS. M. Brown
S. M. Brown
RPR. M. Petrone
R. M. Petrone
CMCarl Mendoza
Carl Mendoza
KDK. J. Devito
K. J. Devito

19 November 1999 in Petroleum Geoscience
Verified
Journal Article
Closed access
MGMurray K. Gingras
Murray K. Gingras
SPS. George Pemberton
S. George Pemberton
CMCarl Mendoza
Carl Mendoza
FHFloyd Henk
Floyd Henk
The potential permeability enhancement of a substrate that has been burrowed by a suite of fauna that inhabit geological firmgrounds (i.e. the Glossifungites ichnofacies) is investigated by using computer simulations, laboratory and field measurements to assess the effective permeability of a Pleistocene Glossifungites surface. All the testing methods indicate that the effective permeability of a substrate is markedly enhanced by the presence of sand-filled Glossifungites burrows in the low-permeability substrate. Furthermore, the permeability of these burrowed horizons can be well approximated by using a modified arithmetic mean that accounts for the degree of interconnectivity between burrows. These formulae are robust and, conceptually at least, can be applied to a variety of geological media and burrow configurations.