One of the most popular geophysical methods currently being used to provide information
about the spatial variation of soil properties is electromagnetic (EM) induction. This is …

The alluvial clay plains of the Murray–Darling Basin (MDB) have been extensively
developed for irrigated agricultural production. Whilst irrigation has brought economic …

Electromagnetic parameters of the subsurface such as electrical conductivity are of great
interest for non‐destructive determination of soil properties (eg, clay content) or hydrologic …

In coastal–estuarine agricultural landscapes, shallow and often saline water tables are
problematic because they limit agricultural productivity. To understand the dynamics of …

Salt related problems in soils can refer to an excess of soluble salts (saline soils), a
dominance of exchangeable sodium in the soil exchange complex (sodic soils), or a mixture …

Within the past 10 yr, frequency‐domain electromagnetic (FEM) induction techniques have
become more and more widely used in soil science and hydrology. Each measurement of …

The soil in arid and semi‐arid areas is often markedly saline, which can severely limit
agricultural productivity. Increasingly, geophysical methods are being implemented to map …

Low induction number EMI instruments are able to simultaneously measure a soil's apparent
magnetic susceptibility and electrical conductivity. This family of dual measurement …

The ability to map the spatial distribution of average soil property values using geophysical
methods at the field and district level has been well described. This includes the use of …

Electromagnetic induction (EMI) has been used to characterize the spatial variability of soil
properties since the late 1970s. Initially used to assess soil salinity, the use of EMI in soil …