เอกสารการประชุมวิชาการและเสนอผลงานวิจัย มหาวิทยาลัยทักษิณ ครั้งที่ 19 2552 - page 69

„µ¦ž¦³»
¤ª·
µ„µ¦Â¨³Áœ°Ÿ¨Šµœª·
‹´
¥ ¤®µª·
š¥µ¨´
¥š´
„¬·
– ‡¦´Ê
Šš¸É
19 ž¦³‹Î
µže
2552
The flexural strength, 30 MPa, was two times higher than that of the conventional materials. The fired specimens
were characterized with respect to the Thai standard specification (TIS 41-1986) as well as bulk density, volume
changes and firing weight loss. The anhydrite, cristobalite, quartz, akermanite, wollastonite and diopside phases
were found by XRD of sintered specimens. The result of study indicated that the batch containing 80% BQD and
20% GOPFA fired at 1200
q
C exhibited the most satisfying ceramic properties that meet the TIS requirements for
making floor tile.
Keywords
:
Basalt quarry dust, Oil palm fiber ash, Industrial wastes, Ceramic tile, Flexural strength
‡Î
µœÎ
µ
®·
œ³Ž°¨˜r
Áž}
œ®·
œ°´
‡œ¸
¡»
ÁœºÊ
°¨³Á°¸
¥— n
ªœ¤µ„¸
Ášµ™¹
Š—Î
µ œÊÎ
µ˜µ¨Â„¤Â—Š ¤n
ªŠžœ—Î
µ Á„·
—‹µ„®·
Ϩϼ
—
…¹Ê
œ¤µÁ¥È
œ˜´
ªœ¡ºÊ
œÃ¨„×¥°µ«´
¥¦°¥Â˜„…°ŠÁž¨º
°„è„®¦º
°ž¨n
°Š£¼
Á…µÅ¢ Ž¹É
ŠÁž}
œ°Š‡r
ž¦³„°®¨´
„…°Š¦¦—µ
Á„µ³Äœ¤®µ¤»
š¦Â¨³n
ªœž¦³„°š´É
ªÅžÄœ£µ‡¡ºÊ
œšª¸
žÁn
œ„´
œ (—œ»
¡¨, 2549) °Š‡r
ž¦³„°šµŠÁ‡¤¸
°°„ÅŽ—r
š¸É
Î
µ‡´
 ŗo
„n
Ž·
¨·
„µ °³¨¼
¤·
œµ Á®¨È
„ ‡¨ÅŽ˜r
¤„œ¸
Ŏ˜r
¨³š¸É
Î
µ‡´
¦°Š¨Š¤µ ŗo
„n
Ηµ ášÁŽ¸
¥¤ ŚšµÁœ¸
¥¤
¨³Â¤Š„µœ¸
¨³¢°¢°¦´
®¦º
°¡·
‹µ¦–µœ·
—¦n
ž¦·
¤µ–œ·
—˜n
µŠÇ ŗo
„n
Á¢¨—r
žµ¦r
¡¨‹·
ðÁ‡¨Â¨³Å¡¦°„
Ž¸
œ ž„˜·
¦n
°°Å‹˜r
(augite) Áž}
œÂ¦n
Î
µ‡´
°´
œ—´
¦°Š µŠ‡¦´Ê
Š¤´
„ž¦µ„’ªn
µ¤¸
¤„œ¸
Ś˜r
ð¨·
ª¸
œ (olivine) ¨³Â¦n
¦°Š
œ·
—°ºÉ
œÇ žœ°¥¼n
—o
ª¥ (—œ»
¡¨, 2552) ®·
œ³Ž°¨˜r
Ĝž¦³Áš«Åš¥¡Áž}
œ®·
œ˜o
œ„Î
µÁœ·
—¦n
¡¨°¥Äœ‹´
Š®ª´
—„µ‹œ»
¦¸
¡¦n
¨Î
µžµŠ «¦¸
¬³Á„¬ ‹´
œš»
¦¸
¨³˜¦µ— n
ªœ®·
œ³Ž°¨˜r
Ťn
Įo
¡¨°¥¡Äœ‹´
Š®ª´
—Á¸
¥Š¦µ¥ ¨Î
µžµŠ Á¡¦¼
¦–r
¨¡»
¦¸
œ‡¦¦µ¸
¤µ ¨»
¦¸
¦³»
¦¸
°»
š´
¥›µœ¸
»
¦¸
¦´
¤¥r
°»
¨¦µ›µœ¸
¨³»
¦·
œš¦r
Ĝ¨´
„¬–³£¼
Á…µÅ¢—´
œ·
šÂ¨o
ª
®·
œ³Ž°¨˜r
Â¥„°°„°Š„¨»n
¤Ä®n
‡º
° „¹É
ŠÂ°¨‡µÅ¨Â¨³Â°¨‡µÅ¨ „¨»n
¤Â¦„ž¦³„°—o
ª¥®·
œ³Ž°¨˜r
žœÃš¨·
Å°˜r
¨³®·
œ³Ž°¨˜r
‡¨„r
-°¨‡µÅ¨ (tholeiitic and calc-alkaline basalts) n
ªœ„¨»n
¤š¸É
°Š‡º
° ®·
œ³Ž°¨˜r
°¨‡µÅ¨
¨³®·
œ³Ž°¨˜r
°¨‡µÅ¨-ð¨·
ª¸
œ ‹ª™¹
Šž{
‹‹»
´
œ®·
œ„n
°¦o
µŠn
ªœ¤µ„čo
®·
œ³Ž°¨˜r
žœÃš¨·
Å°˜r
®¦º
°®·
œÅ—°³
Á (diabase) ÁœºÉ
°Š‹µ„¤¸
‡ªµ¤®œº
—¼
Š„ªn
µ‹¹
Š¤¸
¨´
„¬–³ÂœªÃœo
¤¨—„µ¦˜„Ÿ¨¹
„˜µ¤›¦¦¤µ˜·
Ĝ°¸
„—o
µœ®œ¹É
Š®·
œ³
Ž°¨˜r
°¨‡µÅ¨¤¸
‡ªµ¤®œº
—˜ÉÎ
µÁ®¤µ³¤„´
„µ¦Ÿ¨·
˜ª´
—»
ÁŽ¦µ¤·
„°Ÿœ¹
„¨³Â„o
ªÁŽ¦µ¤·
„ n
ªœÄ®n
œÎ
µ®·
œ¤µÄo
Šµœ
„n
°¦o
µŠ ×¥‡´
—®·
œ³Ž°¨˜r
ÁœºÊ
°Ã¡¦Š…n
µ¥ (vesicular basalt) ¨³˜³„¦´
œ£¼
Á…µÅ¢ (scoria) °°„ °»
˜µ®„¦¦¤„µ¦
Ÿ¨·
˜®·
œÁ¡ºÉ
°„µ¦„n
°¦o
µŠœ·
—œ¸Ê
¤¸
¤µ„Äœ¡ºÊ
œš¸É
£µ‡˜³ª´
œ°°„ÁŒ¸
¥ŠÁ®œº
°˜°œ¨n
µŠ Ž¹É
Š…µ—‡¨œ®·
œ„n
°¦o
µŠœ·
—°ºÉ
œ Ž¹É
Š
ž¦³Áš«Åš¥¤¸
ž¦·
¤µ–®¨n
Š®·
œ³Ž°¨˜r
Î
µ¦°Š¡·
¼
‹œr
(proven reserve) 152.8 ¨o
µœ˜´
œ ¨³¤¸
娬n
Š®·
œ«´
„¥£µ¡
(potential reserve) 42252.8 ¨o
µœ˜´
œ (¥Š¥»
š›Â¨³‡–³ 2551) „µ¦Ã¤n
®·
œ³Ž°¨˜r
šÎ
µÄ®o
ŗo
¤ª¨¦ª¤…œµ—˜n
µŠÇ
Î
µ®¦´
Šµœ„n
°¦o
µŠ ×¥ÁŒ¡µ³¤ª¨¦ª¤¨³Á°¸
¥—š¸É
žœ„´
®·
œŸ»
n
ªœœÁ®¨º
°‡ŠÁ®¨º
°°¥¼n
¤µ„ ÁœºÉ
°Š‹µ„¤¸
ž¦·
¤µ–„µ¦Äo
œo
°¥ š¸É
Á¦¸
¥„ªn
µ ®·
œÁ„¨È
—¨³®·
œ »
i
œ (quarry dust) ®·
œÁ„¨È
—¤¸
…œµ—ž¦³¤µ– 5-10 ¤¤. Ĝ…–³š¸É
®·
œ »i
œ¤¸
…œµ—Á¨È
„
˜´Ê
ŠÂ˜n
5 ¤¤. ¨Š¤µ „n
°œ®œo
µœ¸Ê
ŗo
¤¸
„µ¦«¹
„¬µœÎ
µ®·
œ‡ŠÁ®¨º
°¤µÄo
ž¦³Ã¥œr
®¨µ¥ž¦³„µ¦ °µš·
Án
œ ž»l
¥Â„o
—·
œ§š›·Í
Áž}
œ
„¦— „µ¦Ÿ¨·
˜°·
“¨³„¦³ÁºÊ
°ŠÁŽ¦µ¤·
„ (El-Mahllawy, 2008; El-Alfi, 2004) „µ¦šÎ
µ°·
“¤° (Youssef
et al
., 2004)
¨³šÎ
µª·
‹´
¥„´
œ¤µ„Äœ„µ¦Ÿ¨·
˜ÁŽ¦µ¤·
„„o
ª (Yilmaz
et al
., 1996; Abdel-Hameed, and Bakr, 2007; Karamanov
et al
.,
2007)
1...,59,60,61,62,63,64,65,66,67,68 70,71,72,73,74,75,76,77,78,79,...1457
Powered by FlippingBook