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首页> 外文期刊>American Mineralogist >The synthesis of zeolite-P, Linde Type A, and hydroxysodalite zeolites from paper sludge ash at low temperature (80 {degrees}C): Optimal ash-leaching condition for zeolite synthesis
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The synthesis of zeolite-P, Linde Type A, and hydroxysodalite zeolites from paper sludge ash at low temperature (80 {degrees}C): Optimal ash-leaching condition for zeolite synthesis

机译:在低温(80℃)下由纸渣产生的P型,Linde A型和羟基钠沸石合成沸石:合成沸石的最佳除灰条件

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摘要

Typically, the ash from incineration of paper sludge contains a high percentage of Ca in the form of anorthite (CaAl2Si2O8) and gehlenite (Ca2Al2SiO7). The Ca in the sludge originates from calcite that is included in paper as fillers. We applied acid leaching with HCl on the ash to reduce its Ca content. Zeolite was then synthesized from the leached ash through reaction with 2.5 M NaOH solution at 80 °C for 24 hours. The fraction of Ca and Al extracted from the ash correlates with the pH of the leachant. We determined the leachant pH (after 24 hours of leaching) associated with the Ca: Al:Si ratio in the leached ash that provided optimal production of zeolites with high cation-exchange capacity. During acid leaching, gehlenite dissolved out at higher pH than anorthite. In the case of pH > 5, both gehlenite and anorthite remained in the ash, and hydroxysodalite and LTA (Linde Type A) were synthesized in the product. In the case of pH = 1–5 in the leachant, gehlenite dissolved out but anorthite remained in the ash, and LTA and Na-P1 (zeolite-P) were produced. In the case of pH < 1, both gehlenite and anorthite dissolved out, and only Na-P1 was produced. The cation-exchange capacities of the products that contained hydroxysodalite, LTA, and Na-P1 were approximately 130, 200, and 120 cmol/kg, respectively. We conclude that acid leaching of paper sludge ash controls which of the three zeolite phases form, and that LTA and Na-P1 exhibit a higher cation-exchange capacity than hydroxysodalite. The most efficient production of zeolites with high cation-exchange capacity (about 220 cmol/kg) is obtained after leaching the sludge ash in solutions of around pH = 3. At this low pH, gehlenite has already dissolved out of the sludge ash, half the Ca content of the ash has been leached out, Si has not yet been leached, but Al has begun to be leached. After ash zeolitization, LTA coexists with Na-P1 in the product.
机译:通常,焚烧纸浆产生的灰分含有 高钙钙矿为钙长石(CaAl 2 Si 2 O 8 和钠钙石(Ca 2 Al 2 SiO 7 )。污泥中的Ca 来自方解石,方解石作为填料包含在纸中。我们在灰分上用HCl酸溶 酸以降低其Ca含量。 然后通过与2.5 M NaOH反应的 从沥出的灰中合成沸石溶液在80°C下放置24小时。从灰分中提取的钙和铝的含量 浸出液的pH相关。我们确定了与浸出灰分中的Ca:Al:Si比有关的浸出液pH(浸出24小时后),可以最佳地生产高阳离子交换率的沸石 容量。在酸浸过程中,钙长石在 pH上的溶解度高于钙长石。在pH> 5的情况下,在灰烬中残留有粗斜晶石 和钙长石,并且在产物中合成了羟基钠钙石和LTA (林德A型)。在浸出液中pH值为1-5的情况下,白云母溶解了,但钙锰矿仍留在灰中,而LTA和Na-P1(沸石-P) 已生成。在pH <1的情况下,钠长石和 钙长石都溶解了,仅生成了Na-P1。含有羟基苏打石,LTA, 和Na-P1的产品的阳离子交换 容量分别约为130、200和120 cmol / kg。 < / sup>我们得出结论,纸浆污泥灰分的酸浸控制 这三个沸石相中的哪一个形成,并且LTA和Na-P1 表现出更高的阳离子交换能力 污泥中的灰分浸出后,可以最有效地生产高阳离子交换容量(约220 cmol / kg)的沸石。 pH值约为3的溶液。在这种低pH值下,钠铅矿 已经从污泥中溶解出来,灰分中的一半Ca含量 已经被滤出,Si已经尚未被浸出, ,但是Al已经开始被浸出。灰化后,LTA 与产品中的Na-P1共存。

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  • 来源
    《American Mineralogist》 |2004年第12期|00001694-00001700|共7页
  • 作者单位

    Graduate School of Human and Environmental Studies, Kyoto University, Yoshida-nihonmatsu-cho, Sakyo-ku, Kyoto, Japan;

    Graduate School of Human and Environmental Studies, Kyoto University, Yoshida-nihonmatsu-cho, Sakyo-ku, Kyoto, Japan;

    Access Network Service Systems Laboratories, Nippon Telegraph and Telephone Corporation, Hanabatake, Tsukuba, Japan;

    Graduate School of Human and Environmental Studies, Kyoto University, Yoshida-nihonmatsu-cho, Sakyo-ku, Kyoto, Japan;

    Graduate School of Human and Environmental Studies, Kyoto University, Yoshida-nihonmatsu-cho, Sakyo-ku, Kyoto, Japan;

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