Chemical garden

The chemical garden was first observed and described by Johann Rudolf Glauber in the 17th century i.e., in 1646. In its original form, the chemical garden involved the introduction of ferrous chloride (FeCl₂) crystals into a solution of potassium silicate (K₂SiO₃). However, they were not studied in detail until the 2000s.

Chemical gardens have attracted increasing scientific interest because they can mimic geological and biological structures. Their nonequilibrium behaviour provides model systems for investigating self-organization and hypotheses about the emergence of life on earth and mars. Hydrothermal vent chimneys are regarded as natural analogues of chemical gardens and have been widely studied as models for studying origins of life.

Chemical gardens are named for their plant-like appearance and growth. The study of these structures and related self-organized systems is known as "chemobrionics", an emerging interdisciplinary field that integrates the concepts of physics, chemistry, materials science, biology and complex systems science to investigate reaction-diffusion-driven pattern formation. The term chemobrionics derives from "chemo" and the Greek word bruein ("to grow or enlarge"), referring to the osmotically driven growth of chemical gardens and related self-organized inorganic systems.

Process

Chemical gardens rely on most transition-metal silicates being insoluble in water and colored. When a metal salt, such as cobalt chloride, is added to a sodium silicate solution, it will start to dissolve. It will then form insoluble cobalt silicate by a double displacement reaction. This cobalt silicate is a semipermeable membrane. Because the ionic strength of the cobalt solution inside the membrane is higher than that of the sodium silicate solution, which forms the bulk of the tank contents, osmotic effects will increase the pressure within the membrane. This will cause the membrane to rupture, forming a hole. The cobalt cations will react with the silicate anions at this opening to form a new solid. In this way, growths will form in the tanks; they will be colored (according to the metal cation) and may look like plant-like structures. The growth of chemical gardens is governed by the combined effect of osmotic pressure and buoyancy-driven convection. Osmotic pressure across the semipermeable membrane increases the internal pressure until the membrane ruptures, while buoyancy driven flow promotes the upward growth of the tubular structures.

The usual upward growth direction depends on the density of the fluid inside the semipermeable membrane of the "plant" being lower than that of the surrounding waterglass solution. If a metal salt produces a very dense fluid inside the membrane, growth is downward. For example, a green solution of trivalent chromium sulfate or chloride refuses to crystallize without slowly changing into the violet form, even if boiled until it concentrates into a tarry mass. When suspended in the waterglass solution, that tar forms downward twig-like growths. This is because all the fluid inside the membrane is too dense to float and thereby exerts a downward force. The concentration of sodium silicate becomes important in growth rate.

After the growth has ceased, the sodium silicate solution can be removed by a continuous addition of water at a very slow rate. This prolongs the life of the garden.

In one specific experimental variation, researchers produced the chemical garden with a single growth "tube".

In many modern chemical garden growth experiments, the solid reactant seed is replaced by the continuous injection of the corresponding reactant solution at a controlled flow rate, or more recently, under controlled osmotic pressure.