2009年10月31日星期六

term1 Zaha Hadid's stalactite sculpture











Zaha Hadid shows in New York City some of her (their) most interesting models and installations on December to November, 2008. An exhibition of parametric works that try to mix the concept of Architecture/Sculpture, removing the functionality/location of the project to reinvent them has art pieces.

The strength of the show is that the works cover the major categories these furniture/installation/interventions/space blobs and exploring even as they attempt to blur the line between furniture, sculpture and architecture.

Stalactites, clusters of big chunks suspended from the celling, cuts the gallery space up, guiding traffic, creating eddies to pause in, and with the low lighting in the final installation creates some wonderful shadows.

2009年10月26日星期一

term1 stalactie and stalactite cave



Stalactites are formed by the deposition of calcium carbonate and the other minerals, which is precipitated from mineralized water solutions. Limestone is calcium carbonate rock which is dissolved by water that contains carbon dioxide, forming a calcium bicarbonate solution. This solution travels through the rock until it reaches an edge and if this is on the roof of a cave it will drip down. When the solution comes into contact with air the chemical reaction that created it is reversed and particles of calcium carbonate are deposited.
Every stalactite begins with a single mineral-laden drop of water. When the drop falls, it leaves behind the thinnest ring of calcite. Each subsequent drop that forms and falls deposits another calcite ring. Eventually, these rings form a very narrow, hollow tube commonly known as 'soda straw' stalactite. Soda straws can grow quite long, but are very fragile. If they become plugged by debris, water begins flowing over the outside, depositing more calcite and creating the more familiar cone-shaped stalactite. The same water drops that fall from the tip of a stalactite deposit more calcite on the floor below, eventually resulting in a rounded or cone-shaped stalagmite.

The stalactite cave has fairly stable climate conditions and the relative humidity level is usually close to 100%. So there are lots of water droplets which contained carbonate ion and bicarbonate radical ion in the roof of the cave, also in the air. On the other hand, a report published by the 'National Geographic' mentioned there are lots of caves in the world, and many of them have not been found.

I think if we can use the natural stalactite cave to form architecture space (like cave-dwelling in China), it can create some strange and fantastic space which we are not familiar with. Also, it can solve some public problems like land constraints.













2009年10月18日星期日

term1 salt crystal experiments


I have done some experiments about the salt crystal and consider the factors that influence the crystallization. I heated the saturated solution and it can accelerate the crystallization in a short time. I also add acid into the solution, and the final result can be changed (the color). So, those phenomenons mentioned high temperature and chemical composition can influence the crystallization.

2009年10月14日星期三

term1 crystallization and fossilization

1.crystallization

The crystallization process consists of two major events, nucleation and crystal growth. Nucleation is the step where the solute molecules dispersed in the solvent start to gather into clusters, on the nanometer scale (elevating solute concentration in a small region), that becomes stable under the current operating conditions. These stable clusters constitute the nuclei. However, when the clusters are not stable, they redissolve. Therefore, the clusters need to reach a critical size in order to become stable nuclei. Such critical size is dictated by the operating conditions (temperature, supersaturation, etc.). It is at the stage of nucleation that the atoms arrange in a defined and periodic manner that defines the crystal structure --- note that 'crystal structure' is a special term that refers to the relative arrangement of the atoms, not the macroscopic properties of the crystal (size and shape), although those are a result of the internal crystal structure.

The crystal growth is the subsequent growth of the nuclei that succeed in achieving the critical cluster size. Nucleation and growth continue to occur simultaneously while the supersaturation exists. Supersaturation is the driving force of the crystallization, hence the rate of nucleation and growth is driven by the existing supersaturation in the solution. Depending upon the conditions, either nucleation or growth may be predominant over the other, and as a result, crystals with different sizes and shapes are obtained (control of crystal size and shape constitutes one of the main challenges in industrial manufacturing). Once the supersaturation is exhausted, the solid-liquid system reaches equilibrium and the crystallization is complete, unless the operating conditions are modified from equilibrium so as to supersaturate the solution again.

Many compounds have the ability to crystallize with different crystal structures, a phenomenon called polymorphism. Each poly morph is in fact a different thermodynamic solid state and crystal poly morphs of the same compound exhibit different physical properties, such as dissolution rate, shape (angles between facets and facet growth rates), melting point, etc. For this reason, polymorphism is of major importance in industrial manufacture of crystalline products.

For crystallization to occur from a solution it must be supersaturated. This means that the solution has to contain more solute entities (molecules or ions) dissolved than it would contain under the equilibrium (saturated solution). This can be achieved by various methods. 1. solution cooling or heating. 2. addition of a second solvent to reduce the solubility of the solute. 3. chemical reaction. 4. change in PH being the most common methods used in industrial practice. Other methods, such as solvent evaporation, can also be used.

2. fossilization

The fossilization process: life---death---preservation---survival---discovery

Fossilization potential (FP --- the likelihood of being found as a fossil).

Life: high chance of burial + low in the food chain = high FP (with bonuses for already buried).
low chance of burial + high in the food chain = low FP
Death: smothering by storm or flood sedimentation = high FP
being eaten or rolled around = low FP
Preservation: rapid burial and hard parts = high FP
slow burial and no hard parts = low FP
Survival: burial below sea level and burial in sinking basin shallow burial = high FP
burial above sea level and deep burial = low FP
Discovery: a fossil cannot be discovered unless the sedimentary rock containing it is exposed at the Earth's surface.