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Development and calibration of a novel sensor to quantify the water content of surface soils and biological soil crusts
Author(s) -
Weber Bettina,
Berkemeier Thomas,
Ruckteschler Nina,
Caesar Jennifer,
Heintz Henno,
Ritter Holger,
Braß Henning
Publication year - 2016
Publication title -
methods in ecology and evolution
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 3.425
H-Index - 105
ISSN - 2041-210X
DOI - 10.1111/2041-210x.12459
Subject(s) - soil water , environmental science , biogeochemical cycle , water content , soil science , nutrient , substrate (aquarium) , arid , soil horizon , atmosphere (unit) , hydrology (agriculture) , environmental chemistry , atmospheric sciences , ecology , geology , chemistry , meteorology , geotechnical engineering , biology , physics
Summary The surface layer of soil as transition zone between pedosphere and atmosphere plays a crucial role in exchange processes of nutrients, atmospheric gases and water. Knowledge of its water content is essential, as it governs both physiological and transport mechanisms. In arid and semi‐arid regions, this uppermost soil layer is commonly colonized by biological soil crusts (biocrusts), which play major roles in the global terrestrial carbon and nitrogen cycles. The water status of biocrusts is essential as it controls the activity, productivity and surface exchange of these poikilohydric communities. On‐site analyses of the water content of both bare and crusted soils are thus urgently needed to correctly model the exchange processes of water, nutrients and trace gases at the soil surface. In this study, we present the biocrust wetness probe ( BWP ), which is the first to reliably measure the water content within biocrusts or the uppermost 5 mm of a substrate. Using a weak alternating current, the electrical conductivity is assessed over time. With an automatic calibration routine, conductivity values are temperature‐corrected and converted into water contents and precipitation equivalents. During 1 year of continuous field measurements at 5‐min intervals, 60 BWP s worked reliably without any failure. The probes responded immediately and individually upon rain events, showing substrate‐specific water response curves, which are well represented by linear and exponential calibration curves. The BWP facilitates the spatio‐temporal assessment and interpolation of surface soil wetness and thus biocrust activity, which governs nutrient fluxes, trace gas release and biogeochemical cycles. Its implementation in distributed sensor networks is under development.