Hydrothermal laboratory

A small volume batch reactor
'Big Rig' a large column flow-through apparatus

This laboratory is used to study chemical reactions between fluids and rocks under conditions found in the top few kilometres of the Earth's crust. In its 25+ years it has been at the centre of numerous investigations that require well-controlled conditions to study reaction processes under in-situ conditions (i.e. elevated temperatures and pressures), and it is probably unique in the range of very different studies that have been investigated in the laboratory.

Background

The laboratory was set up at Harwell in 1979 when the UK high-level radioactive waste programme needed to understand reactions between vitrified waste and groundwater. In 1983 it was dismantled and moved to the BGS main site at Keyworth.

The high-level waste programme ceased in 1981, and the laboratory was then used to study how hot granite reacted with water as part of the hot dry rock (HDR) geothermal programme in Cornwall. Knowledge gained from this facilitated study of reactions in geothermal systems in Costa Rica (1985–87) and and within submarine black smokers (as part of the British mid-ocean ridge (BRIDGE) initiative (1994–95)).

The demise of the UK HDR programme in 1989 led to another shift in activities, studying the impacts of cement-based materials as engineered barriers for the disposal of radioactive wastes. The laboratory was a major source of information on the way in which alkaline cement porewaters react with rocks, for both UK and international programmes (1989-2000).

In 1992 concern about the effect of carbon dioxide (CO2) on global temperatures resulted in BGS leading an international team investigating the potential for the deep underground storage of CO2.

Within this programme, and similar ones that continue today, the laboratory was used to study reactions between CO2, groundwaters and rock types that might be encountered during the deep underground storage of CO2. Other current activities also include weathering processes and how metals are leached from mine waste.

Capabilities

Static (batch) and flow-through equipment are available in the laboratory, with useable volumes ranging from less than one millilitre to over ten litres. Much of the equipment can withstand high temperatures and pressures, with current standard operating conditions up to about 400°C and 500 bar.

More extreme conditions can be simulated with with minor modifications. Although some equipment is 'off the shelf', numerous pieces are novel, having been specially developed for the laboratory. The experimental reaction products are characterised using a wide range of fluid chemical and mineralogical analytical techniques that are available within other dedicated laboratories at the BGS.

High pressure optical cell
Rocking autoclave - assembled rocking high pressure reactor

The Big Rig

The 'Big Rig' and experimental set-up

BGS has developed an in-house laboratory capability to carry out experiments simulating fluid-rock interactions in deep geological conditions. Experiments utilise a specialised pressure vessel, the 'Big Rig' (Figure 1).

Geological materials to be investigated are packed into a titanium column (100 cm long with an internal diameter of 3.6 cm) which in turn is loaded into the Big Rig. The confining pressure is maintained by a syringe pump. Reactant fluid is equilibrated in a 3 litre conditioning vessel before being displaced into the column. Fluid pressure and flow are further controlled by syringe pumps. Samples of the reactant fluid are collected from the column using a floating-piston titanium pressure sampler.

Relevance to important issues

Experiments produce data relevant to important issues of today:

  • studying the high temperature alteration of borosilicate glass, an important waste-form being considered for the for disposal of high-level radioactive waste
  • investigating the reactions occurring in and around highly alkaline cement, with a view to understanding alkaline disturbed zones around repositories for the underground disposal of low-intermediate radioactive waste
  • quantifying the reactivity of CO2 with rocks, and its impact on long-term mineral trapping during the deep underground disposal of CO2
  • studying reactions occurring within high temperature geothermal systems, and their potential impact on rocks and reservoir properties
  • investigating weathering processes, including the leaching of toxic metals from fly ash and mine wastes
  • quantifying the dissolution rates of a variety of minerals in order to help improve the accuracy and confidence in predictive geochemical computer models

Contact

Please contact Keith Bateman or Chris Rochelle for further information