Wednesday, March 25, 2009
PMA - JKR Experiance
Sunday, March 15, 2009
INFO Kerja Penurapan Jalan
"JALAN YANG BARU DITURAP DAN SELESAI DIGELEK TIDAK BOLEH DIBUKA KEPADA TRAFIK SEHINGGA BAHAN TURAPAN TELAH SEJUK. PADA KEBIASAANNYA TIDAK KURANG DARIPADA EMPAT JAM(4 JAM) SELEPAS DIGELEK"
Saturday, March 14, 2009
Polymer Modified Asphalt (PMA)
Info From "http://www.semmaterials.com/"
What, How, Why?
- the polymer system used
- the compatibility of the polymer with the asphalt.
Why modify?
Improvement in resistance to rutting, thermal cracking, fatigue damage, stripping, and temperature susceptibility have led polymer modified binders to be substituted for asphalt in virtually all paving and maintenance applications, including hot mix, warm mix - cold lay, cold mix, chip seals, hot and cold crackfilling, patching, recycling, and slurry seal. They are used wherever extra performance and durability are desired. In many cases they are selected to reduce life cycle costs. Polymer modified binders have allowed the use of techniques previously not practicable, such as micro-surfacing and using emulsion chip seals on high traffic roads.
Tuesday, March 10, 2009
Rocks
abstract from " A Guide to good quality control practices on asphalt production and construction"
Rocks are classified relative to their geological origins and these are termed Igneous, Sedimentary and metamorphic
1. Igneous Rocks
formed from hot liquid or magma, cooling either above or beneath the earth's surface.
examples are Grannite & basalt
2. Sedimentary Rocks
The action of wind or water on a rocks surface results in the formation of smaller particles. These particles are deposited on river or sea beds or depressions in the earth's surface. This sediment accumulates and is buried. Compaction and cementation over the years removes the air and water to form sedimentary rocks.
Typical example is Limestone
3. Metamorphic rocks
Heat, pressure and chemical substances deep beneath the earth's surface act on existing igneous and sedimentary rocks to form a new type called metamorphic rocks, example marble