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 Encyclopedia of Physical Science and Technology  EN002J-63  May 18, 2001  14:16






               196                                                                     Biomineralization and Biomimetic Materials


               sponge, Monoraphis, that is attached to the seabed by a  faces. These work in concert with the supply of calcium
               large silica rod, 1 m long. The structure of this material is  and carbonate from the mantle tissue. The mantle adds
               a series of concentric layers where the weaker interlayer  new shell at the existing edge by extruding over the lip to
               regions may enhance the toughness of the structure, like  extend the outer and inner faces.
               a laminated glass windshield.                       The vaterite form of calcium carbonate often occurs
                 Siliceous diatoms are single-celled prokaryotes, about  in laboratory crystallization and is occasionally found in
               100 µm in diameter, enclosed by a porous silica shell,  shells. There is increasing evidence for precipitation of
               in the form of two overlapping dishes, like a petri dish.  amorphous, hydrated calcium carbonate as a metastable
               The organism multiplies by dividing into two disc-shaped  precursor for the crystal. In some cases, including lobster
               cells and then forming two new dishes back-to-back. The  cuticle and a sponge, stable amorphous calcium carbonate
               cells then separate, each with one new half shell and one  is found.
               old one. Recent work on the proteins involved in silica
               mineralization has started to clarify the details of silica
                                                                 C. Hydroxyapatite
               deposition in diatoms and sponges. Plants often contain
               silica as a reinforcing material, and the structure of bam-  The human body is supersaturated for both calcium car-
               boo has been much studied in this context. Seawater and  bonate and for hydroxyapatite, Ca 10 (OH) 2 (PO 4 ) 6 , the
               soil water contain low levels of dissolved silica as sili-  mineral of bone and tooth. Since the environmental avail-
               cic acid, which the cell probably binds and transports as  ability of phosphorus is limited, its use as a reinforcement
               a complex with catechols (dihydroxybenzene) and then  seems peculiar. Possibly bone acts a phosphorus reservoir.
               converts this to silica nanoparticles.            Boneisessentiallyapolymer-matrixcompositereinforced
                                                                 with ribbons of hydroxyapatite. The structure and proper-
                                                                 ties of bone are discussed by Currey et al. (1995). A key
               B. Carbonate
                                                                 current question is the way the lamellar structure gives rise
               Calcium carbonate is widespread as a protective shell  to a combination of high stiffness, high strength, and high
               in marine animals, from single-celled coccoliths through  toughness. Similar synthetic composites tend to break at
               coral, gastropods, and bivalves. It also occurs as a rein-  relatively low strain and so have low toughness.
               forcement in the cuticle of crustaceans such as crabs. The  Dentine has a structure similar to bone but with signifi-
               use of calcium carbonate for shells, rather than silica, may  cantdifferencesinthemechanismofmineralization.Tooth
               reflect the greater control of structure available through  enamel is almost wholly mineral with a fibrous structure
               calcium-binding proteins and through control of crystal  that forms under the control of a completely different set
               morphology with nucleators and growth inhibitors. Silica  of mineralization proteins, including amelogenin.
               does occur as a component of many mollusk teeth, as do
               various iron oxides.
                 There has been much recent work on the formation,  V. BIOLOGICAL AND SYNTHETIC
               structure, and properties of mollusk shell. Most shells are  PROCESSING
               constructed of calcite and aragonite in various arrange-
               ments with small amounts of protein, up to about 5% by  In practical engineering, where cost is very important,
               weight. Higher protein levels would be expected to in-  there is little sense in designing a part without a very good
               crease the toughness of the shell but at the expense of  idea of how it will actually be made. Materials selections
               reduced stiffness. It can be assumed that particular shell  are then made once the manufacturing route and basic
               structures are adapted to the particular lifestyles of the an-  design have been decided. The same must be true in biol-
               imals and the stresses encountered. For instance, it might  ogy; many interesting structural features may be primarily
               be expected that a swimming bivalve, such as a scallop,  a consequence of the growth process and only secondarily
               would have a stiffer, lighter shell structure. One of the most  a source of improved properties.
               studied shell structures is nacre, or mother-of-pearl, which  Small numbers of synthetic parts can be made by sub-
               is a layered structure of aragonite plates, 0.5 µm thick by  tractive processes such as machining but the process is
               several microns wide. Between each layer of plates is a  slow and wasteful. Molding is generally cheaper and
               thin protein sheet that is responsible for nucleation of the  faster. Hot liquid material is injected into a hollow tool and
               aragonite layers and acts as a crack stopper, which gives  allowed to solidify. Extrusion, forging, rolling, and other
               wet nacre a very high fracture energy.            hot processes can be viewed as variants on molding. The
                 While the details of shell formation are not understood,  sintering of ceramics is a separate case; compacted powder
               it is clear that organic content contains proteins capable of  isheateduntilsurfaceenergydrivestheslowshrinkageand
               selectively nucleating calcite or aragonite in a specific ori-  densification to a solid. Chemical processing is not com-
               entation and proteins that inhibit growth of specific crystal  mon in the synthetic world. Thermosetting resins such as
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