2015 - Fellow of American Geophysical Union (AGU)
The scientist’s investigation covers issues in Weathering, Mineralogy, Silicate, Paleontology and Dissolution. Her Weathering research is multidisciplinary, incorporating perspectives in Soil science, Soil water, Dilution and Chemical composition. In her study, which falls under the umbrella issue of Soil science, Organic matter and Soil production function is strongly linked to Hydrology.
Her research integrates issues of Drainage basin, Carbon cycle, Forcing and Earth science in her study of Mineralogy. Her Silicate research is multidisciplinary, relying on both Tectonics, Volumetric flow rate, Vadose zone, Groundwater and Infiltration. Her studies deal with areas such as Fluid dynamics, Clay minerals and Aquifer as well as Dissolution.
Her primary scientific interests are in Weathering, Geochemistry, Hydrology, Environmental chemistry and Mineralogy. Her Weathering research includes elements of Soil science, Carbon cycle, Earth science and Silicate. The concepts of her Geochemistry study are interwoven with issues in Glacial period and Paleontology.
Her work on Aquifer, Hydrology, Residence time and Drainage basin as part of general Hydrology study is frequently linked to Biogeosciences, bridging the gap between disciplines. Kate Maher focuses mostly in the field of Environmental chemistry, narrowing it down to matters related to Groundwater and, in some cases, Sediment. Within one scientific family, Kate Maher focuses on topics pertaining to Dissolution under Mineralogy, and may sometimes address concerns connected to Plagioclase.
Kate Maher mainly focuses on Soil carbon, Hydrology, Plant phenology, Soil respiration and Montane ecology. The study incorporates disciplines such as Organic matter, Climate change mitigation, Decomposer and Soil management in addition to Soil carbon. Her Groundwater, Infiltration and Aquifer study in the realm of Hydrology connects with subjects such as Riparian zone.
Her primary areas of investigation include Equilibrium fractionation, Isotope fractionation, Redox, Electron transfer and Reaction rate constant. Many of her studies involve connections with topics such as Kinetic fractionation and Equilibrium fractionation.
This overview was generated by a machine learning system which analysed the scientist’s body of work. If you have any feedback, you can contact us here.
Hydrologic Regulation of Chemical Weathering and the Geologic Carbon Cycle
K. Maher;C. P. Chamberlain.
The dependence of chemical weathering rates on fluid residence time
Earth and Planetary Science Letters (2010)
Environmental speciation of actinides.
Kate Maher;John R. Bargar;Gordon E. Brown.
Inorganic Chemistry (2013)
The role of reaction affinity and secondary minerals in regulating chemical weathering rates at the Santa Cruz Soil Chronosequence, California
Kate Maher;Carl I. Steefel;Art F. White;Dave A. Stonestrom.
Geochimica et Cosmochimica Acta (2009)
The mineral dissolution rate conundrum: Insights from reactive transport modeling of U isotopes and pore fluid chemistry in marine sediments
Kate Maher;Carl I. Steefel;Donald J. DePaolo;Donald J. DePaolo;Brian E. Viani.
Geochimica et Cosmochimica Acta (2006)
The role of fluid residence time and topographic scales in determining chemical fluxes from landscapes
Earth and Planetary Science Letters (2011)
Fluid-Rock Interaction: A Reactive Transport Approach
Carl I. Steefel;Kate Maher.
Reviews in Mineralogy & Geochemistry (2009)
Marine anoxia and delayed Earth system recovery after the end-Permian extinction
Kimberly V. Lau;Kate Maher;Demir Altiner;Brian M. Kelley.
Proceedings of the National Academy of Sciences of the United States of America (2016)
Expanding the role of reactive transport models in critical zone processes
Li Li;Kate Maher;Alexis Navarre-Sitchler;Jennifer Druhan.
Earth-Science Reviews (2017)
Persistence of soil organic carbon caused by functional complexity
Johannes Lehmann;Johannes Lehmann;Colleen M. Hansel;Christina Kaiser;Markus Kleber.
Nature Geoscience (2020)
If you think any of the details on this page are incorrect, let us know.
We appreciate your kind effort to assist us to improve this page, it would be helpful providing us with as much detail as possible in the text box below: