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As America Took Time to Celebrate Its Independence and its Tradition as a Beacon of Freedom to the World, the Trump Administration Seized the Moment to Continue Dismantling Immigration and Refugee Programs

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— but one group that’s benefiting is the private prison industry (and their investors).

At the Daily Beast, Betsy Woodruff covered a shareholder call this week conducted by the GEO group, a private prison company that is being sued for human trafficking and whose stock price has tripled since the election of Donald Trump. GEO is the Very Fine Ballroom Salsa Practice Dance Shoes for Women SERA703BBX 15Inch Heel Foldable Brush Bundle Black Suede H40YJ7
to ICE, CBP, and the Marshals Service, and expects to handle at least a quarter of Trump’s planned immigrant detentions. Executives on the shareholder call were nearly gleeful that Trump’s deportation policies will mean more arrests, more detention, and more demand for their services — coming together to create what CEO George Zoley called “culturally responsive environments” for GEO.

GEO’s plans for profit

As Woodruff wrote, GEO iscarefully monitoring announcements and executive actions from Trump and his Administration, translating them into a need for its services, and planning on profiting bigly. GEO is also noting an increase in immigration enforcement in the interior of the US, far away from border regions:

GEO and its relationship to Trump

Woodruff’s piece also describes how GEO is part of Trump’s favor-based economy, its financial ties to Trump, and its ugly human rights record when it comes to those it detains:

Zoley said a new ICE contract for a 1,000-bed detention center in Conroe, Texas, will cost $117 million to build and will generate $44 million in revenue per year once it’s opened in late 2018. The CEO said the company expects “increased demand for detention capacity at the federal level,” and that it bought the Maverick County Detention Center in Texas for $15 million to meet that demand.

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Sedflux

SEDFLUX is a basin-fill model, written in ANSI-standard C, able to simulate the delivery of sediment and their accumulation over time scales of tens of thousands of years. It simulates the dynamics of strata formation of continental margins fuse information from the atmosphere, ocean and regional geology, and it can provide information for areas and times for which actual measurements are not available, or for when purely statistical estimates are not adequate by themselves.

Sedflux combines individual process-response models into one fully interactive model, delivering a multi-sized sediment load onto and across a continental margin. The model allows for the deposit to compact, to undergo tectonic processes and isostatic subsidence from the sediment load. The new version, Sedflux 2.0 introduces a series of new process models, and is able to operate in one of two models to track the evolution of stratigraphy in either 2D or 3D. Additions to the 2D mode include the addition of models that simulate (1) erosion and deposition of sediment along a riverbed, (2) cross-shore transport due to ocean waves, and (3) turbidity currents and hyperpycnal flows. New processes in the 3D mode include (1) river channel avulsion, (2) two-dimensional diffusion due to ocean storms, and (3) two-dimensional flexure due to sediment loading. The spatial resolution of the architecture is typically 1–25 cm in the vertical and 10–100 m in the horizontal when operating in 2D mode. In 3D mode, the horizontal resolution usually extends to kilometers. In addition to fixed time steps (from days to hundreds of years), Sedflux 2.0 offers event-based time stepping as a way to conduct long-term simulations while still modeling low-frequency but high-energy events.

This will be something that the CSDMS facility will add

1) Water discharge

2) Mean suspended load entering the ocean basin

3) Bedload equation by Bagnold (1966)

1) Advection-diffusion equation

2) Froude number

3) Plume's centerline

4) Non-conservative concentration along and surrounding the centerline position

1) Amount of bottom sediments that can be reworked by resuspension and diffusion

2) Amount and direction of transport of the ith grain size

1) Stability of a possible failure plane

2) excess pore pressure using Gibson's graphical approximation (1958)

Fluid continuity equation 1) one dimensional steady-state turbidity current model INFLO

Continuity equation for the ith grain size of the flow's suspeneded load

The rate of erosion of the ith grain size of the seafloor by the current

Rate of deposition of the ith grain size in the flow

Critical velocity for deposition

2) turbidity current model Sakura Governing equation

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