Soil Profile

  • Processor 1

    The most widely used direct method to measure the water content in soil is the thermo-gravimetric method, often assumed as a reference procedure because it uses precise devices. Alternative indirect methods measure a physico-chemical properties from which soil water content is estimated. The most popular is the Time Domain Reflectometry (TDR). Large-scale (> 20 ha) soil water content is estimated through the Cosmic-Ray neutron probe. This detector measures the neutron flux (³He or Boron) within a hypothetical circle of 150 m radius to estimate average soil water content.

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Department of Agraria.

Università degli Studi di Napoli "Federico II"

via Università, 100 - Portici

  • Telephone number: 081 2539421

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