非饱和带土壤水分和稳定同位素剖面。野外观测和分析

Pub Date : 2022-01-01 DOI:10.5200/baltica.2022.2.6
Žana Skuratovič, J. Mažeika, O. Jefanova, R. Petrošius
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引用次数: 0

摘要

本文综述了非饱和土壤剖面中地下水位和水文气象参数变化对土壤水分波动的影响。我们重点观测了土壤含水量、气温、降水和地下水位。采用基于视介电常数变化的ThetaProbe土壤水分传感器进行土壤体积含水量测量。在自然大气条件下,传感器安装在不饱和带剖面的不同深度。观测持续了五年多(2013年11月14日至2018年12月31日)。使用Diver数据记录仪获取地下水位数据,该记录仪连续记录水压和水温。为了更详细地调查Maišiagala放射性废物储存库现场水的水和质量运输,还使用了稳定同位素作为环境示踪剂。
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Soil water and stable isotopes in the unsaturated zone profile – field observations and analysis
In this review, we provide research data emphasizing the role of groundwater table and hydrometeorological parameters variation on soil water fluctuations in the unsaturated soil profile. We focused on soil water content, air temperature, precipitation and groundwater table observations. The ThetaProbe Soil Water Sensors basing on changes in the apparent dielectric constant were used for soil volumetric water content measurements. The sensors were installed at the different depths of the unsaturated zone profile under natural atmospheric conditions. The observations lasted more than five years (14 November 2013 – 31 December 2018). Groundwater table data was obtained using Diver data loggers, which continuously recorded water pressure and temperature. For more detailed investigations of water and mass transport at the Maišiagala radioactive waste repository site water, stable isotopes as environmental tracers were used as well.
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