Geology Reports⌕ Search

USGS · tm6A56

Documentation for the “XT3D” option in the Node Property Flow (NPF) Package of MODFLOW 6

Abstract

This report describes the “XT3D” option in the Node Property Flow (NPF) Package of MODFLOW 6. The XT3D option extends the capabilities of MODFLOW by enabling simulation of fully three-dimensional anisotropy on regular or irregular grids in a way that properly takes into account the full, three-dimensional conductivity tensor. It can also improve the accuracy of groundwater-flow simulations in cases in which the model grid violates certain geometric requirements. Three example problems demonstrate the use of the XT3D option to simulate groundwater flow on irregular grids and through three-dimensional porous media with anisotropic hydraulic conductivity. Conceptually, the XT3D method of estimating flow between two MODFLOW 6 model cells can be viewed in terms of three main mathematical steps: construction of head-gradient estimates by interpolation; construction of fluid-flux estimates by application of the full, three-dimensional form of Darcy’s Law, in which the conductivity tensor can be heterogeneous and anisotropic; and construction of the flow expression by enforcement of continuity of flow across the cell interface. The resulting XT3D flow expression, which relates the flow across the cell interface to the values of heads computed at neighboring nodes, is the sum of terms in which conductance-like coefficients multiply head differences, as in the conductance-based flow expression the NPF Package uses by default. However, the XT3D flow expression contains terms that involve “neighbors of neighbors” of the two cells for which the flow is being calculated. These additional terms have no analog in the conductance-based formulation. When assembled into matrix form, the XT3D formulation results in a larger stencil than the conductance-based formulation; that is, each row of the coefficient matrix generally contains more nonzero elements. The “RHS” suboption can be used to avoid expanding the stencil by placing the additional terms on the right-hand side of the matrix equation and evaluating them at the previous iteration or time step. The XT3D option can be an alternative to the Ghost-Node Correction (GNC) Package. However, the XT3D formulation is typically more computationally intensive than the conductance-based formulation the NPF Package uses by default, either with or without ghost nodes. Before deciding whether to use the GNC Package or XT3D option for production runs, the user should consider whether the conductance-based formulation alone can provide acceptable accuracy for the particular problem being solved.

Explore related subjects

Keep this discovery

Explore connections, maps & timelines

BibTeXRIS

Alden M. Provost, Christian D. Langevin, Joseph D. Hughes. 2017-08-10. Documentation for the “XT3D” option in the Node Property Flow (NPF) Package of MODFLOW 6. https://doi.org/10.3133/tm6a56

Cite the original work for its findings. Save a collection to share your selection of sources.

KEEP EXPLORING

Related USGS reports

Methods and considerations for writing science syntheses for use in decision making on public lands

Natural resource managers are required by multiple laws to use science to inform decisions on public lands in the United States. However, large numbers of science papers about conservation and management of natural resources are published annually, increasing the amount of effort required to maintain awareness of the best available science on relevant topics. As a result, products that synthesize large bodies of science can be a key tool for communicating science to natural resource managers. This report provides guidance for writing synthesis products for resource managers. Core topics and steps include coproducing syntheses with managers, scoping topics relevant to management actions and potentially affected resources, using reproducible literature search and screening methods, extracting and synthesizing multiple types of management-relevant information from science papers, organizing the synthesis product according to decision-making processes, soliciting peer and end-user review, and planning dissemination activities tailored to resource managers. Considering these topics and steps in developing science synthesis products can facilitate natural resource managers’ ability to use science in decision making and help bridge the gap between research and public land management.

Techniques and Methods↗

An updated decision-support tool for grassland birds in the Avian-Impact Offset Method

The Avian-Impact Offset Method (AIOM) quantifies the displacement of grassland birds and waterfowl in response to energy infrastructure and estimates the amount of habitat needed to compensate for this loss. The AIOM converts the number of bird pairs lost owing to avian behavioral avoidance (also referred to as “displacement”) and estimates the site-specific hectares of grasslands or number of wetlands needed to compensate for displaced pairs of grassland birds or waterfowl, respectively. Decision-support tools spatially apply the AIOM to estimate grassland and wetland offsets and guide the location of offsetting measures. The revised decision-support tool for grassland birds and grassland offsets described in this report provides updated grassland layers for calculating offsets and updated bird models for guiding the location of offsetting measures.

Techniques and Methods↗

dMODELS, a MATLAB software package for modeling crustal deformation near volcanic centers and active faults using Global Navigation Satellite System data—User guide

dMODELS is a MATLAB software package that implements the most common analytical models used to interpret deformation measurements near faults and active volcanic centers. This manual focuses on inversion of deformation data from the Global Navigation Satellite System (GNSS). The included case studies emphasize the GNSS inversion component of the software. Source models include pressurized spherical, spheroidal, and horizontal sill (penny-crack) magma reservoirs in a homogeneous, elastic, isotropic, flat half-space. A topography correction is available for the spherical source. Dikes and faults are described following the mathematical notation for the rectangular dislocations in a homogeneous, elastic, flat half-space. Equations have been reviewed for typographical errors present in the original literature and verified against finite-element method numerical models. GNSS data from the 2006 eruption at Augustine Volcano, Alaska; the 1998–2000 unrest at Taal Volcano, Philippines; and the 2009 earthquake in L’Aquila, Italy, are used to demonstrate the application of the software package.

Techniques and Methods↗