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JoVE Journal
Chemistry
Chemical Gardens as Flow-through Reactors Simulating Natural Hydrothermal Systems
Chemical Gardens as Flow-through Reactors Simulating Natural Hydrothermal Systems
JoVE Journal
Chemistry
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JoVE Journal Chemistry
Chemical Gardens as Flow-through Reactors Simulating Natural Hydrothermal Systems

Chemical Gardens as Flow-through Reactors Simulating Natural Hydrothermal Systems

Full Text
15,004 Views
12:55 min
November 18, 2015

DOI: 10.3791/53015-v

Laura M. Barge1,2,3, Yeghegis Abedian1,2, Ivria J. Doloboff1,2, Jessica E. Nuñez1,3,4, Michael J. Russell1,2, Richard D. Kidd1, Isik Kanik1,2

1NASA Jet Propulsion Laboratory,California Institute of Technology, 2NASA Astrobiology Institute,Icy Worlds, 3Blue Marble Space Institute of Science, 4Citrus College

Overview

This article describes the formation of chemical gardens through laboratory simulations that mimic natural systems found at submarine hydrothermal vents. The experiments aim to recreate the self-assembling structures characteristic of these environments.

Key Study Components

Area of Science

  • Neuroscience
  • Biochemistry
  • Geochemistry

Background

  • Chemical gardens are structures formed by the precipitation of minerals.
  • They can provide insights into early Earth conditions.
  • Submarine hydrothermal vents are key locations for studying these processes.
  • Understanding these formations can shed light on the origins of life.

Purpose of Study

  • To simulate natural chimney formations at submarine hydrothermal vents.
  • To generate self-assembling structures on a small scale.
  • To investigate the chemical processes involved in these formations.

Methods Used

  • Preparation of two solutions: one simulating early Earth seawater and the other simulating alkaline hydrothermal fluid.
  • Setting up an apparatus for fluid injection under an anoxic atmosphere.
  • Measuring voltage between hydrothermal and ocean solutions during injection.
  • Injecting the hydrothermal-like solution into the simulated ocean solution.

Main Results

  • Successful simulation of natural seepage of vent fluid.
  • Observation of self-assembling structures resembling chemical gardens.
  • Data on voltage changes during the injection process.
  • Insights into the conditions that favor chemical garden formation.

Conclusions

  • The experiments effectively mimic natural processes at hydrothermal vents.
  • Findings contribute to understanding the origins of life on Earth.
  • Further research could explore the implications of these structures in early Earth chemistry.

Frequently Asked Questions

What are chemical gardens?
Chemical gardens are structures formed by the precipitation of minerals in a solution, often resembling plant-like shapes.
Why are submarine hydrothermal vents important?
They are key locations for studying the chemical processes that may have contributed to the origins of life on Earth.
How does the experiment simulate early Earth conditions?
By preparing solutions that mimic the composition of early Earth seawater and hydrothermal fluids.
What measurements are taken during the experiment?
Voltage measurements are taken between the hydrothermal and ocean solutions during the injection process.
What insights can be gained from this research?
The research provides insights into the conditions that favor chemical garden formation and their implications for early Earth chemistry.

We describe chemical garden formation via injection experiments that allow for laboratory simulations of natural chemical garden systems that form at submarine hydrothermal vents.

The overall goal of the following experiment is to simulate natural chimneys precipitated at submarine hydrothermal vents of early earth using chemical garden experiments to generate the self assembling structures on a small scale. This is achieved by first preparing two solutions. One solution simulates the composition of early earth seawater, and one solution simulates an alkaline hydrothermal fluid produced by water rock reactions.

Next, an apparatus is set up so that the hydrothermal like fluid can be injected into a reservoir of the simulated ocean under an anoxic atmosphere. As a third step, electrodes are set up to measure the voltage between hydrothermal and ocean solutions during the injection. Finally, the hydrothermal like solution is slowly injected into the base of a vial containing the simulated ocean solution, mimicking the natural seepage of vent fluid out of the ocean crust and into the surrounding sea water.

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