本帖最後由 kenwong 於 2016-5-25 01:01 編輯
http://www.youtube.com/watch?v=wPjqo6Ad1Gw
http://www.youtube.com/watch?v=2IA8T3GXqBU
http://baike.baidu.com/view/915187.htm
蛭石保水力保肥力皆高於珠石
但會隨時間瓦解堅變泥降低通氣性
珠石是將玻璃質打散開而成
基本上是完全chemically inert 的東西
用以保持泥土結構
蛭石是一層又一層帶 -ve charge plate夾著ion的千層糕 是以保肥
http://cpl.usu.edu/files/publications/factsheet/pub__7320194.pdf
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Vermiculite's strong buffer capacity renders it unsuitable for studies of acidity on soybean (Glycine max L.) nodulation and growth.
http://www.ncbi.nlm.nih.gov/pubmed/24229409
聽聞有一定 中性 pH buffering 能力....個人未有求証過
"Buffering ability of vermiculite was also shown by Duman and Tunç [15] when water of different pH (2.20, 3.0, 5.95, and 10.58) was added to vermiculite substrate. The initial pH value of water was adjusted to 2.20, 3.0, 5.95, and 10.58 by adding HCl or NaOH before preparation of vermiculite/water suspension. Then, vermiculite was added on it and the pH value of the suspension was recorded at various time intervals. Vermiculite increased acid suspension pH from 2.20 to 2.24, from 3.0 to 5.77, from 5.95 to 9.79; and slightly decreased alkaline pH from 10.58 to 10.10 after 180 minutes. Similar to our finding, it is shown here that buffering capacity of vermiculite decreased when the pH of water was very acid (2.20) or very alkali (10.58).
The increase of suspension pH by vermiculite was caused by the adsorption of H+ ions from solutions to the negatively charged surface of vermiculite. As explained by Duman and Tunç [2] vermiculite layers have permanent negative charges; but when the pH of solution was very alkali, the transfer of protons from SiOH (or AlOH) groups in the lattice of vermiculite to free OH- ions with formation of H2O in the suspension may cause a decrease in pH value."
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