The Role of Reactive Transport Modeling in Geologic Carbon Storage

The engineered storage of CO2 in Earth’s subsurface provides one of the most promising means of reducing net greenhouse gas emissions. Paramount to the success of this method is ensuring that CO2 injected into the subsurface is securely stored. Reactive transport models can be used to answer the key question regarding CO2 storage, “Will the injected CO2 be secure, and over what timescale?” Here, we explore examples of how reactive transport models have been used to simulate the range of geochemical and hydrologic processes that will take place over thousands of years and across many spatial scales to answer that key question.

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December 2025 --The Variscan Orogeny in Europe – Understanding Supercontinent Formation

The Variscan orogen formed between 380 and 300 million years ago through several accretionary and collisional cycles, culminating with the construction of the Pangea supercontinent. This process occurred via sequential opening and closure of oceanic basins, synchronous detachment of Gondwana derived continental ribbons, and their outboard amalgamation onto the Laurussia margin. The Variscan orogen is rather unique compared with other orogenic belts on Earth: its overthickened and dominantly magmatic crust in the central belt, surprisingly minor mantle involvement in the magmatic and geodynamic processes, coherent and pulsed magmatism along the collision suture, and its complex accretionary history. Because its final product, Pangea, is the youngest and best-understood supercontinent on Earth, the Variscan orogeny offers clues for understanding the mechanisms of supercontinent formation.