Author name: Susan L. Brantley

Crossing Disciplines and Scales to Understand the Critical Zone

The Critical Zone (CZ) is the system of coupled chemical, biological, physical, and geological processes operating together to support life at the Earth’s surface. While our understanding of this zone has increased over the last hundred years, further advance requires scientists to cross disciplines and scales to integrate understanding of processes in the CZ, ranging in scale from the mineral–water interface to the globe. Despite the extreme heterogeneities manifest in the CZ, patterns are observed at all scales. Explanations require the use of new computational and analytical tools, inventive interdisciplinary approaches, and growing networks of sites and people.

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Reactive Transport Models of Weathering

Continental rocks chemically weather when surficial waters and gases interact with the minerals and organisms that inhabit Earth’s critical zone. To understand and quantify this process, researchers use reactive transport models to track the kinetics and thermodynamics of weathering reactions and the transport of products and reactants. These models are powerful tools to explore how weathering sculpts the Earth’s surface from the scale of mineral grains to watersheds, and across temporal scales from seconds to millions of years. Reactive transport model simulations are now a vital tool for elucidating the complex links between climate, rock ­weathering, and biota.

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