Relationship between electrical conductivity and water content of peat and gyttja: implications for electrical surveys of drained peatlands

Abstract

The application of electrical resistivity tomography to peatlands supports conventional coring by providing data on the current condition of peatlands, including data on stratigraphy, peat properties and thickness of organic deposits. Data on the current condition of drained peatlands are particularly required to improve estimates of carbon storage as well as losses and emissions from agriculturally used peatlands. However, most of the studies focusing on electrical resistivity tomography surveys have been conducted on natural peatlands with higher groundwater levels. Peatlands drained for agriculture have not often been studied using geophysical techniques. Drained sites are characterized by low groundwater levels and high groundwater fluctuations during the year, which lead to varying levels of water saturation. To validate better electrical resistivity tomography surveys of drained peatlands, the aim of this laboratory study is to investigate the influence of varying water saturation levels on electrical conductivity (reciprocal of resistivity) for a variety of peat and gyttja types, as well as for different degrees of peat decomposition. Results show that different levels of water saturation strongly influence bulk electrical conductivity. Distinct differences in this relationship exist between peat and gyttja substrates and between different degrees of peat decomposition. Peat shows an exponential relationship for all degrees of decomposition, whereas gyttja, in particular organic‐rich gyttja, is characterized by a rather unimodal relationship. The slopes for the relationship between electrical conductivity and water content are steeper at high degrees of decomposition than for peat of low degrees of decomposition. These results have direct implications for field electrical resistivity tomography surveys. In drained peatlands that are strongly susceptible to drying, electrical resistivity tomography surveys have a high potential to monitor the actual field water content. In addition, at comparable water saturations, high or low degrees of decomposition can be inferred from electrical conductivity.

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Imaging Tropical Peatland and Aquifer Potential in South Sumatera Using Electrical Resistivity Tomography

“…Groundwater level also affects the physical properties of the peat. (Walter, Lück, Heller, Bauriegel, & Zeitz, 2019) have shown that different levels of water saturation strongly influence bulk electrical conductivity (reciprocal of resistivity). In dry season groundwater level fall far below the surface, thereby decreasing moisture contents of the surface peat and creating vast amounts of dry fuel that are a fire hazard (Wösten, Clymans, Page, Rieley, & Limin, 2008).…”

Geomorphometric and Geophysical Constraints on Outlining Drained Shallow Mountain Mires

“…Using three different mires located over the Stolowe Mountains (central Sudetes) we tested the application of integrating digital elevation models, remote sensing data and shallow geophysical prospecting methods (electrical resistivity tomography and ground penetrating radar) to delineate the extent of mires, their thickness, internal structure, and basement morphology. Our approach was guided by the effectiveness of those geophysical methods proven in investigations on other wetlands [10][11][12][13][14][15][16], the proven applicability of remote sensing in the analysis of diversity of vegetation and monitoring of changes in biodiversity [17,18], as well as the analytical potential of LiDAR-based DTM shown for the Stolowe Mountains National Park in Poland [19].…”