A mountain-scale model for characterizing unsaturated flow and transport in fractured tuffs of Yucca Mountain
A mountain-scale model for characterizing unsaturated flow and transport in fractured tuffs of Yucca Mountain (in Research advances in vadose zone hydrology through simulations with the TOUGH codes, Stefan Finsterle (editor) and Curtis M. Oldenburg (editor))
Vadose Zone Journal (August 2004) 3 (3): 796-805
- aquifers
- boundary conditions
- Cenozoic
- fracturing
- ground water
- heterogeneous materials
- high-level waste
- hydrology
- igneous rocks
- infiltration
- Miocene
- movement
- Neogene
- Nevada
- numerical models
- Nye County Nevada
- Paintbrush Tuff
- percolation
- porous materials
- pyroclastics
- rates
- scale models
- Tertiary
- three-dimensional models
- Tiva Canyon Member
- Topopah Spring Member
- tracers
- transport
- tuff
- United States
- unsaturated zone
- volcanic rocks
- waste disposal
- waste disposal sites
- Yucca Mountain
- Calico Hills Formation
- Crater Flat Group
We present a large-scale modeling study characterizing fluid flow and tracer transport in the unsaturated zone (UZ) of Yucca Mountain, Nevada, the proposed underground repository site for storing high-level radioactive waste. The modeling study is conducted using a three-dimensional numerical model, which incorporates a wide variety of field data and takes into account the coupled processes of flow and transport in Yucca Mountain's highly heterogeneous, unsaturated, fractured porous rock. The modeling approach is based on a dual-continuum formulation. Using different conceptual models of unsaturated flow, various scenarios of current and future climate conditions and their effects on the UZ are evaluated to aid in the assessment of the repository's system performance. These models are calibrated against field-measured data. Model-predicted flow and transport processes under current and future climates are discussed.