Variation of Moisture and Soil Water Retention in a Lowland Area of Central Poland—Solec Site Case Study

Soil moisture monitoring is crucial for a variety of activities involving soil water regime estimation. Different phenomena such as drought, exhibit impacts of a variable extent in the soil profile, requiring moisture content monitoring as well as reliable analyses of the soil properties. In the village of Solec, located in central Poland, monitoring of the moisture content was attempted for a sandy soil in order to estimate soil moisture distributions for two dry years (2015, 2016) and a wet one (2017). Simple and easily obtainable drought indices, such as dry spells, climatic water balance, groundwater table depth, soil water content and potential were estimated and related with spatiotemporal evolution of soil water conditions. Soil layers subject to drought were found to be different either from a moisture (15–45 cm) or soil water potential (10–25 cm), showing diverse physical properties and relations with the ground water table. The coherence of the analysed drought indices was proven for a light, sandy soil, which has national significance for the state, drought monitoring network. Knowledge obtained during previous studies, which omitted soil water conditions for this type of the soil was supplemented. Based on its own water content, the profile of the analysed soil (Stagnic Folic Gleysols–Arenic) exhibits a negative climatic water balance and requires irrigation practices to mitigate drought effects.