Chemistry: analytical and immunological testing – Geochemical – geological – or geothermal exploration – For metallic ores
Reexamination Certificate
2001-08-08
2004-02-03
Warden, Jill (Department: 1743)
Chemistry: analytical and immunological testing
Geochemical, geological, or geothermal exploration
For metallic ores
C436S080000, C436S086000, C436S172000, C436S525000, C502S403000
Reexamination Certificate
active
06686202
ABSTRACT:
FIELD OF THE INVENTION
This invention relates generally to the use of non-naturally occurring specific gold-binding proteins or peptides for use in analytic, exploration or recovery methods in the gold mining industry.
BACKGROUND OF THE INVENTION
Gold is one of the rarest precious metals on earth. It occurs naturally as the reduced metal (Au°) or associated with quartz or pyrites as telluride (AuTe
2
), petzite (AuAg)
2
Te or sylvanite (AuAg)Te
2
. The electronics and space industries use gold's properties of electrical conductivity and heat reflection. Gold has applications in radar equipment, home computers, satellites and space exploration. Gold is also used in considerable quantities in the form of gold leaf (having a thickness of less than 0.2 &mgr;m) for sign writing and book binding lettering. Gold film has been used in glass windows to reflect heat. Liquid gold is a suspension of very finely divided gold particles in vegetable oil that is used in the decoration of china articles. Gold salts are used for toning in photography, and in coloring glass.
Most frequently gold in nature is dispersed in low concentration throughout large volumes of material, usually rock. Gold deposits occur in belts across the earth's crust in various forms: placers or quartz veins in sedimentary or indigenous formation, blanket or pebble beds or conglomerates, or as base metal ore associations. Gold occurs in ore bodies described as lodes or veins, replacement deposits, contact (skarn) deposits, volcanogenic deposits, deposits associated with intrusive activity (such as ‘porphyry’ systems and breccia pipes) and deposits associated with ferruginous sediments (banded iron formations) and cherts. Gold bearing veins are found in rocks of all compositions and geologic ages, deposited in cavities and associated with rocks such as slates or schists. Lode deposits consist of gold particles contained in quartz veins or country rock. Lode deposits usually are mined in deep underground mines using a variety of methods, although sometimes lode deposits are surface mined. The blanket or reef-type deposits are deposits in which the gold exists in quartz conglomerates. Disseminated gold deposits have three identifying characteristics. The gold mineralization is fairly evenly distributed throughout the deposit rather than being concentrated in veins (as in lode deposits) or in pay-streaks (as in placer deposits); the deposits consist of in place materials rather than transported materials; and the disseminated deposits are less flat. Generally, these types of deposits are mined using surface mining techniques.
Gold also exists in secondary ore deposits. All rock outcrops exposed at the surface of the earth are subjected to the natural elements of weathering and erosion, causing eventual breakdown of rock into fragments which are carried away by wind, water or ice. The fragments are then redeposited in river systems, lakes or in the sea. During the erosive cycle, the heavier and more durable gold is concentrated into rich deposits, even though the original rock may have contained low values. Residual deposits of gold are found close to the gold bearing outcrop after the other rock fragments have weathered and been carried away. Eluvial deposits are formed when gold or gold bearing rock fragments have been transported short distances from their source (generally by gravity) and have been concentrated within the soil horizon. Alluvial deposits are formed by the concentration of gold particles within stream systems, under the action of running water. Beach placers, where gold is concentrated in beach sands by wave action, are a type of alluvial deposit. Leads are former stream courses, containing gold, where barren sands have covered the original passage of the stream. Deep leads are gold deposits in former stream beds which have been covered with basaltic lava. Nuggets are formed, either as rich fragments of primary deposits which have been transported and deposited in a sedimentary environment, or a chemical accretion of small gold particles into larger fragments. Some nuggets may have formed through the chemical action of host soils or sediments on a gold solution. Placer deposits are flat-laying deposits composed of unconsolidated materials, such as gravel and sands, in which the gold particles occur as free particles ranging in size from nuggets to fine flakes. They are the result of erosion and transport of rock. Placer deposits most commonly are mined using water based surface methods, including hydraulic methods, dredging and open pit mining. These deposits usually are not mined in underground operations.
Methods for recovering gold from its ores (termed “beneficiation methods”) are extremely expensive and labor and heavy machinery intensive. Gold is one of the least reactive metals on earth. It does not combine with oxygen or with nearly any other chemicals, no matter how corrosive. Some gold ores are free milling and allow the separation of coarse gold using methods that depend on the high specific gravity of gold. All other commonly used methods depend on the use of cyanide which is highly toxic, hazardous to the environment and difficult to remove. Basically, the first step in all methods is to subject the ore to cyanide leaching followed by a gold recovery process. The three known methods for extracting gold from the cyanide leach solution are the “Merrill-Crowe” or zinc dust precipitation process, the carbon-in pulp process, and the carbon in-leach process. Other gold recovery processes use gravity methods to extract the high proportion of free gold and flotation-roasting leaching to extract the remaining gold.
Cyanide and cyanide by-products from cyanide leaching operations are responsible for several environmental impacts, including air and water pollution and solid waste disposal contamination. Free cyanide and various cyanide complexes are the by products of current leaching methods. Although cyanide will degrade, for example in a surface stream exposed to ultraviolet light, aeration and complexing with various chemicals present in the stream water, in-stream degradation is a wholly unsatisfactory approach to removing cyanide from the environment. Cyanide solutions are often kept in open ponds and frequently birds or other animals are exposed and killed by the toxic material.
Air pollution with cyanide also is an unavoidable result of prior art methods for heap-leaching of gold. Cyanide solutions are sprayed onto the heaps, the cyanide drifts and contaminates the surrounding environment. As is the case with cyanide released into water, eventually the cyanide is degraded by ultraviolet light, but not until after it has adversely affected the environment. The EPA directs considerable efforts and expense in regulating cyanide releases into the air and water. Chronic cyanide toxicity due to long-term exposures to low levels is also a health factor to be considered, and the effects such exposures are not presently well known. For these reasons there has been a long standing need for gold mining processes which do not pollute the environment with cyanide and cyanide byproducts.
Gold recovery from secondary sources such as electronic scrap and waste electroplating solutions, as well as recovery from primary sources such as leach solutions is also an important technology. Various processes such as carbon adsorption, ion exchange, membrane separation, precipitation, and solvent extraction have been used for isolation of metal ions, including gold.
Recently, methods for the utilization of naturally occurring proteins or biologic materials in analytic or gold recovery, including microbial biomass, as an adsorbent for metals have been studied. Bontideau et al.,
Anal. Chem.
70:1842-1848 (1997) is a physical chemical study of the two-dimensional binding properties between a naturally occurring protein and a gold substrate. The arrangement and enzymatic activity of a myosin sub-fragment were characterized with special focus on the direct attachment of the thiol groups of cysteines in the protein
Chevillon Victor
Clendenning James B.
Furlong Clement E.
Jorgenson-Soelberg Scott
Kirshenbaum Noel W.
Cole Monique T.
Placer Dome Inc.
Swanson & Bratschun LLC
Warden Jill
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