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Dosseto, A., Hesse, P., Maher, K., Fryirs,
K. and Turner, S.P. (submitted) Climatic control of continental erosion
via
climate induced vegetation shift. In review.
Fantle, M. S. and Maher, K. (submitted) Isotopic Approaches
for Quantifying the Rates of Marine Burial Diagenesis. Reviews in Geophysics.
Maher, K. (submitted)
The dependence of chemical weathering rates on fluid residence time.
Maher, K. Steefel, C. I, Stonestrom, D. A. and White, A.F. (2009)
The Role of Secondary Minerals and Reaction Affinity in Regulating Weathering
Rates at the Santa Cruz Marine Terrace Chronosequence. Geochimica et Cosmochimica
Acta, 73, 2804-2831.
Singer D. M., Maher K., and Brown, G.E. Jr. (2009) Uranyl-chlorite
sorption/desorption: Evaluation of different U(VI) sequestration processes.
Geochim. Cosmochim. Acta 73, 5989-6007.
Steefel, C.I.,
K. Maher (2009) Fluid-rock interaction: A reactive transport approach.
Reviews in Mineralogy and Geochemistry 70: 485-532,
DOI: 10.2138/rmg.2009.70.11.
White, A. F.
Schulz, M. S., Stonestrom, D. A., Vivit, D. V., Fitzpatrick, J., Bullen,
T., Maher, K. and Blum, A.E. (2009) Chemical Weathering
of a Marine Terrace Chronosequence, Santa Cruz, California II: Controls
on
Solute Fluxes and Comparisons of Long-term and Contemporary Mineral
Weathering rates. Geochimica et Cosmochimica Acta, 73, 2769-2803.
Conrad
M. E., DePaolo D. J., Maher K., Gee G. W., Ward A. L.(2007) Field
Evidence for Strong Chemical Separation of Contaminants in the Hanford
Vadose Zone. Vadose Zone Journal 6, 1031-1041.
Maher K., Wooden J.W., Paces J.B., Miller, D. M., (2007).
230Th/U dating of surficial deposits using the ion microprobe (SHRIMP-RG):
a microstratigraphic perspective. Quaternary International, 66 (1), 15-28.
DePaolo, D. J., Maher K., Christensen J. N, McManus, J.R.
(2006) Sediment transport time measured with U-series isotopes: results
from ODP North Atlantic Drift Site 984. Earth and Planetary Science Letters,
248 (1-2), 379-395.
Maher K., Christensen J. N, DePaolo D. J., (2006) U-Sr isotopic
speedometer: Flow and chemical weathering rates in aquifers. Geochimica
et Cosmochimica Acta 70 (17), 4417-4435.
Maher
K., Steefel C. I., and DePaolo D. J. (2006) The mineral dissolution
rate conundrum: insights from reactive transport modeling of U isotopes
and pore fluid chemistry. Geochimica Et Cosmochimica Acta 70(2),
337-363.
Singleton
M.J., Maher K., DePaolo D.J., Conrad M.E., and Dresel P.E. (2006).
Regional flow and recharge of the unconfined aquifer at Hanford, WA from groundwater
isotopic compositions. Journal of Hydrology 321, 39-58.
Maher
K., DePaolo D. J., and Lin J. C. F. (2004a) Rates of silicate
dissolution in deep-sea sediment: In situ measurement using U-234/U-238
of pore fluids. Geochim. Cosmochim. Acta 68(22), 4629-4648.
Christensen
J. N., Dresel P. E., Conrad M. E., Maher K., and Depaolo
D. J. (2004) Identifying the sources of subsurface contamination at the
Hanford Site in Washington using high-precision uranium isotopic measurements. Environ.
Sci. Technol. 38(12), 3330-3337.
DePaolo
D. J., Conrad M. E., Maher K., and Gee G. W. (2004) Evaporation
effects on oxygen and hydrogen isotopes in deep vadose zone pore fluids
at Hanford, Washington: Implications for recharge and horizontal fluid
movement. Vadose Zone Journal 3, 220-232
Maher
K., DePaolo D. J., Conrad M. E., and Serne R. J. (2003) Vadose
zone infiltration rate at Hanford, Washington, inferred from Sr isotope
measurements. Water Resources Research 39(8), 1029-1043 |
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