Low–temperature specific heat capacity of water--ammonia mixtures down to the eutectic: applications in geodynamic modelling of icy moons
Robust thermodynamic data are essential for the development of geodynamic and geochemical models of ocean worlds. The water–ammonia system is of interest due to its purported abundance in the outer solar system, geological implications and potential importance for origins of life. In support of deve...
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sg-ntu-dr.10356-1657592023-04-12T06:27:24Z Low–temperature specific heat capacity of water--ammonia mixtures down to the eutectic: applications in geodynamic modelling of icy moons Chua, Bing Hong Benoit Taisne Asian School of the Environment Jet Propulsion Laboratory, California Institute of Technology Steven Vance Mathieu Choukroun mohit.melwani.daswani@jpl.nasa.gov Science::Chemistry::Physical chemistry::Thermodynamics Robust thermodynamic data are essential for the development of geodynamic and geochemical models of ocean worlds. The water–ammonia system is of interest due to its purported abundance in the outer solar system, geological implications and potential importance for origins of life. In support of developing new equations of state, we conducted 1bar specific heat capacity measurements (Cp) using a differential scanning calorimeter at low temperatures (184−314K) and low mass fractions of ammonia (5.2−26.9wt%) to provide novel data in the parameter space relevant for planetary studies. This is the first known set of data with sufficient fidelity to investigate the trend of specific heat capacity with respect to temperature. The obtained Cp in the liquid phase domain above the liquidus increases with temperature. Deviations of our data from the currently adopted equation of state by Tillner-Roth and Friend are negative (ranging from +1% to −10%) and larger at lower temperatures. This result suggests that suppression of the critical behavior of super-cooled water (rapid increase in specific heat with decreasing temperature) by ammonia starts at a smaller concentration than that set by Tillner-Roth and Friend. Cp measurements of the liquid were also obtained in the partial melting domain between the eutectic and liquidus. This novel dataset will be useful in future investigations of conditions where such partial melt may exist, such as the ice shell– ocean boundary or the interiors of ocean worlds that may contain relatively large proportions of dissolved ammonia. Bachelor of Science in Environmental Earth Systems Science 2023-04-10T06:36:58Z 2023-04-10T06:36:58Z 2023 Final Year Project (FYP) Chua, B. H. (2023). Low–temperature specific heat capacity of water--ammonia mixtures down to the eutectic: applications in geodynamic modelling of icy moons. Final Year Project (FYP), Nanyang Technological University, Singapore. https://hdl.handle.net/10356/165759 https://hdl.handle.net/10356/165759 en application/pdf Nanyang Technological University |
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Science::Chemistry::Physical chemistry::Thermodynamics Chua, Bing Hong Low–temperature specific heat capacity of water--ammonia mixtures down to the eutectic: applications in geodynamic modelling of icy moons |
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Robust thermodynamic data are essential for the development of geodynamic and geochemical models of ocean worlds. The water–ammonia system is of interest due to its purported abundance in the outer solar system, geological implications and potential importance for origins of life. In support of developing new equations of state, we conducted 1bar specific heat capacity measurements (Cp) using a differential scanning calorimeter at low temperatures (184−314K) and low mass fractions of ammonia (5.2−26.9wt%) to provide novel data in the parameter space relevant for planetary studies. This is the first known set
of data with sufficient fidelity to investigate the trend of specific heat capacity with respect to temperature. The obtained Cp in the liquid phase domain above the liquidus increases with temperature. Deviations of our data from the currently adopted equation of state by Tillner-Roth and Friend are negative (ranging from +1% to −10%) and larger at lower temperatures. This result suggests that suppression of the critical behavior of super-cooled water (rapid increase in specific heat with decreasing temperature) by ammonia starts at a smaller concentration than that set by Tillner-Roth and Friend. Cp measurements of the liquid were also obtained in the partial melting domain between the eutectic and liquidus. This novel dataset will be useful in future investigations of conditions where such partial melt may exist, such as the ice shell–
ocean boundary or the interiors of ocean worlds that may contain relatively large proportions of dissolved ammonia. |
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Benoit Taisne |
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Benoit Taisne Chua, Bing Hong |
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Final Year Project |
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Chua, Bing Hong |
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Chua, Bing Hong |
title |
Low–temperature specific heat capacity of water--ammonia mixtures down to the eutectic: applications in geodynamic modelling of icy moons |
title_short |
Low–temperature specific heat capacity of water--ammonia mixtures down to the eutectic: applications in geodynamic modelling of icy moons |
title_full |
Low–temperature specific heat capacity of water--ammonia mixtures down to the eutectic: applications in geodynamic modelling of icy moons |
title_fullStr |
Low–temperature specific heat capacity of water--ammonia mixtures down to the eutectic: applications in geodynamic modelling of icy moons |
title_full_unstemmed |
Low–temperature specific heat capacity of water--ammonia mixtures down to the eutectic: applications in geodynamic modelling of icy moons |
title_sort |
low–temperature specific heat capacity of water--ammonia mixtures down to the eutectic: applications in geodynamic modelling of icy moons |
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Nanyang Technological University |
publishDate |
2023 |
url |
https://hdl.handle.net/10356/165759 |
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1764208131221487616 |