Report header & site
Traverses on map
Active Β· Point A
β , β
Active Β· Point B
β , β
Bearing AβB
β
βm β active traverse length (used for spacing)
Add a traverse for each sounding line. Tap or GPS sets A/B on the active traverse; tap a line on the map to make it active. Every traverse is drawn with its length; all of them go into the Word report's location plan.
Base map & offline tiles
βtiles
Offline storage used
β
Service worker
β
Pan and zoom to your site while you still have signal, choose how many zoom levels deep to cache, then download. Tiles and the app shell are stored on-device so the map renders β and the report's map image composes β with no connection. The Word report reuses these cached tiles, so download your area before you lose signal. Requires HTTPS or localhost.
Recommended probe spacing (active traverse)
βm
Basis
aβββ = L / 3
Approx. investigation depth
β
Wenner electrodes sit at 0, a, 2a, 3a β so the outer current pins span 3a. The AβB line is taken as the widest reading (C1βC2 at aβββ); smaller spacings nest symmetrically about the AβB midpoint. Depth of investigation β a (median depth β 0.5a per Edwards). Min spacing and step ratio are shared across traverses; aβββ follows each traverse's own length.
Ambient conditions (site)
Fetched once for the whole site (centroid of all traverse points). Soil resistivity tracks moisture and temperature; recent rain lowers readings, dry or frozen ground raises them. Weather is a live call and won't refresh offline β fetch it before you lose signal.
Measurements β apparent resistivity
Input mode
Save / export
Field aid only β always confirm spacing series, array footprint, and interpretation against IEEE Std 81 and the requirements of your grounding study (e.g. CDEGS RESAP soil model). Apparent resistivity assumes a homogeneous half-space at each spacing; layered structure is resolved during model fitting, not in the field. Data is stored locally in this browser. Weather via open-meteo.com (no key). Base map Β© OpenStreetMap contributors.