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wenzhou leya hardware Co.Ltd
wenzhou leya hardware Co.Ltd Professionally engaged in metal hardware
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Leya alloy cabinet handle metal drawer pull Ref 6006 color Nickel plated/Satin Nickel

wenzhou leya hardware Co.Ltd
wenzhou leya hardware Co.Ltd
City: Beijing
Province/State: Beijing
Country/Region: China
Tel: 86-10-67163047
Contact Person:
Mr Brady Sumer

Leya alloy cabinet handle metal drawer pull Ref 6006 color Nickel plated/Satin Nickel

Brand Name : Leya
Model Number : 6006
Certification : CCPIT CE etc
Place of Origin : China
MOQ : 2000 pcs
Price : US$1.08 -1.35/pcs
Payment Terms : L/C, T/T, Western Union
Supply Ability : 500,000
Delivery Time : 1 month
Packaging Details : Carton
Color : Silver
Material : ZAMAK (zinc alloy)
More color : Gold,Silver,Bronze and others
Surface : Satin Nickel/ Gold / Satin Gold (Special color negotiable)
Usage : Furniture and cabinet
Style : Modern simple
Origin : China
Weight : 62-83g (referenced)
Contact Now

MAIN INFORMATION:

Product name: Zamak furniture handle
Brand: Leya
Product Number: 6006
Manufactured by: Wenzhou Leya Metal Hareware.Co.,Ltd
The subsidiary of Sumer (Beijing) International Trading Co.,Ltd

PRODUCT DETAIL:

Type: Simple style
Material: Zamak (Zinc alloy)
Usage: Cabinet,drawer, dresser kitchen or other furniture hardware use.
Color: Gold,Silver,Bronze and others
Surface :Satin Nickel/Chrome Plated (Special color negotiable)
Central space: 96 / 128 mm (special spec negotiable)
Weight: 62-83 g (for your reference)
Product origin:China
Packing: Carton

MAIN FEATURE:


Good quality and reasonable price.
Directly from Factory;
Customers’ design welcome;

MORE INFORMATION:

Zinc Minerals
The most commonly found zinc mineral is sphalerite (ZnS) also known as zinc blende, which is found in almost all currently mined zinc deposits. The mineral crystallizes from the hydrothermal solution as pure zinc sulfide.
The mineral marmatite is a complex zinc-iron sulfide, which is commonly found but rarely exploited, as it is not easy to smelt.
Zinc deposits close to the earth’s surface are often converted to oxides and carbonates. Small quantities of zinc carbonate – the mineral calamine (smithsonite) in North America – often refer to the hydrated silicate mineral also known as hemimorphite.
Iron and lead sulfides, in the form of the minerals pyrite and galena are always associated in significant quantities while smaller quantities of other metals are commonly found.
Metamorphically formed oxide zinc ores such as franklinite or zincite are limited to only a few deposits.
Zinc is a natural component of the earth’s crust and an inherent part of our environment. Zinc is present in rock, soil, air, and water. Plants, animals and humans also contain zinc.
The average natural level of zinc in the earth’s crust is 70 mg/kg (dry weight), ranging between 10 and 300 mg/kg (Malle 1992).
In some areas, zinc has been concentrated to much higher levels by natural geological and geochemical processes (5-15% or 50,000-150,000 mg/kg). Such concentrations, found at the earth’s surface and underground, are being exploited as ore bodies.

In the early 1930s Morris Ashby in Britain had licensed the New Jersey zamak alloy. The high-purity refluxer zinc was not available in Britain and so they acquired the right to manufacture the alloy using a locally available electrolytically refined zinc of 99.95% purity. This was given the name Mazak, partly to distinguish it from zamak and partly from the initials of Morris Ashby. In 1933, National Smelting licensed the refluxer patent with the intent of using it to produce 99.99% zinc in their plant at Avonmouth.


Zinc Deposits
Zinc ore deposits are widely spread throughout the world. Zinc ores are extracted in more than 50 countries. Australia, Canada, China, India, Peru and Europe are the largest producers. Zinc is normally associated with lead and other metals including copper, gold and silver. There are four major types of zinc deposits:
1.Volcanic hosted massive sulfides (VMS)
VHMS deposits are polymetallic and are an important economic source of copper and zinc often associated with significant concentrations of silver, gold, cadmium, bismuth or tin.
2.Carbonate hosted (Mississippi Valley & Irish types)
Limestone and dolomite are the most common host rocks. The zinc lead content usually ranges from 5%-10% with zinc usually predominating over lead. Concentrations of copper, silver and barite of fluorite may also be present.
3.Sediment hosted (sedex deposits)
The host rocks are mainly shale, siltstone, and sandstone. Sedex deposits represent some of the world’s largest accumulations of zinc, lead and silver. The mineral has a high silver content. The lead/zinc content ranges from 10-20%.
4.Intrusion related (high sulfidation, skarn, manto, vein)
These deposits are typically found in carbonate rocks in conjunction with magmatic-hydrothermal systems and are characterized by mineral association of calcium and magnesium. Typically the ore body contains more lead than zinc and is associated with silver.


Zamak 3 properties


PropertyMetric valueImperial value
Mechanical properties
Ultimate tensile strength268 MPa38,900 psi
Yield strength (0.2% offset)208 MPa30,200 psi
Impact strength46 J (56 J aged)34 ft-lbf (41 ft-lbf aged)
Elongation at Fmax3%
Elongation at fracture6.3% (16% aged)
Shear strength214 MPa31,000 psi
Compressive yield strength414 MPa60,000 psi
Fatigue strength (reverse bending 5x108 cycles)48 MPa7,000 psi
Hardness97 Brinell
Modulus of elasticity96 GPa14,000,000 psi

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