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Estimation of raised bogs peat moisture

机译:升降沼泽泥炭水分的估计

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The purpose of the research was to study the moisture ratio of peat deposit in natural and drained condition,detection of changes of water characteristics of bogs after forest reclamation.Despite some changes of water -thermal balance of the peat deposit of Site 1 places are not different in peat moisture.The reason is weak influence of drainage of peatland "Vasjuganskoe".That's why it's important to use measures for drainage system restoration and achieving objective of forest reclamation.Peat deposit moisture is defined by a lot of hydro-meteorological factors,structure of peat deposit and type of peat and its botanical composition.That's why additional research is necessary for development of science-based models for assessment of space and time dynamics of moisture.Comparison of moisture characteristics of peat deposit of forest reclamation areas with natural raised bog showed no changes of peat moisture of antropogenically changed bog.
机译:该研究的目的是研究泥炭沉积物的天然和排出条件的水分,检测森林回收后沼泽水的变化。泥炭矿床的一些水分变化1个地方不是泥炭水分不同。原因是泥炭地“瓦斯朱甘蓝山”排水的影响薄弱。这就是为什么利用排水系统恢复和实现森林回收目标的目标是重要的.Peat沉积水分由大量水力气象因素定义,泥炭沉积和泥炭型的结构及其植物组合物。这就是为什么额外研究是为了评估湿度的空间和时间动态的基于科学的模型所必需的额外研究。污水沉积地区的泥炭沉积地区的水分特征和自然饲养沼泽显示没有变化的植物水分变化的沼泽。

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