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首页> 外文期刊>Revista Geologica de America Central >Variations and characteristics in changes of the crater lake level of Irazú volcano (1965-2012), Costa Rica
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Variations and characteristics in changes of the crater lake level of Irazú volcano (1965-2012), Costa Rica

机译:哥斯达黎加Irazú火山火山口湖水位变化的变化和特征(1965-2012)

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The small and ephemeral crater lake of the Irazú has presented noticeable changes in its coloring, temperature, pH, and depth from 1965 until 2012. The level has varied from 31 m in 1995 and 2001 to stay completely dry in 1977, 1979, 1982-83, 1987 and 1990. These levels are not always directly related to the amount of rainfall. It seems that at times the waterproofed base of the lake was cracked allowing the lake to drain relatively quickly, leaving the base visible for several months or years, and after a time, formed again. The variation of the color (green, turquoise-blue, yellow, rare whitish and reddish), temperature (16º-35ºC), and pH (2.85-5.85) seems to be related to the depth, underwater fumarolic activity, algae activity and ferruginous sediments produced by the constant landslides of the walls.
机译:从1965年到2012年,伊拉祖(Irazú)小而短暂的火山口湖的颜色,温度,pH和深度发生了显着变化。水位从1995年的31 m变化到1977年,1979年和1982年保持完全干燥, 83、1987和1990年。这些水平并不总是与降雨量直接相关。似乎湖的防水基底有时会裂开,使湖相对较快地流失,使基底可见数月或数年,然后又形成了。颜色(绿色,蓝绿色,黄色,稀有的白色和红色),温度(16º-35ºC)和pH值(2.85-5.85)的变化似乎与深度,水下富马酸活性,藻类活性和铁质有关墙壁不断滑坡产生的沉积物。

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