Abstract

For the first time, using the example of a key object of the peat river valleys of the Kuznetsk Alatau occupied by spruce forests, it is shown that swamp waters are clearly differentiated by the content of the main ions due to forest–peat fires. Swamp waters objectively form three groups: (1) waters of the original type of mineral nutrition (fresh, soft), (2) waters of peatland covered by a medium fire (fresh, hard), (3) waters of peatland covered by a high fire (slightly saline, very hard). Magnesium ions and bicarbonates have the highest discriminating power (95%) in the determination of swamp waters. The swamp waters of the post-pyrogenic peatland do not lose the ratio of the main ions, which is similar to waters of the original type, and retain the hydro-carbonate calcium–magnesium composition.

中文翻译：

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评估森林-泥炭火灾对富营养化沼泽水化学特性影响的经验

摘要

首次以云杉林占据的库兹涅茨克阿拉套泥炭河谷的一个关键对象为例，表明由于森林-泥炭火灾，沼泽水的主要离子含量明显不同。沼泽水客观上形成三组：（1）原始矿物营养类型的水（新鲜、软），（2）被中火覆盖的泥炭地水（新鲜、硬），（3）被中火覆盖的泥炭地水。高火（略咸，非常硬）。在测定沼泽水时，镁离子和碳酸氢盐具有最高的辨别力 (95%)。后热解泥炭地的沼泽水没有失去主要离子的比例，与原始类型的水相似，并保留了碳酸氢盐钙镁组成。