Sentence examples for soils detection from inspiring English sources

Based on the dielectric constant distinction between frozen and unfrozen soils, Ground Penetrating Radar(GPR) were widely used on frozen soils detection.

Shannon Piper of St .Louis University studies how nanoparticles can be used to extract DNA from soil for detection of soilborne pathogens.

The best soil sealing detection is carried out based on principal component analysis of the images and the SAVI index.

This study aimed to design a simple transducer for soil tilth detection by determining dynamic strain behaviour of commercially available spring tines.

The results of this study can be further extended to other spatial scales and can provide a foundation for soil change detection using upcoming imaging spectroscopy satellite platforms that acquire spatial spectral temporal information.

Other systems discussed are used in soil phosphorus detection using near-infrared (NIR) and Raman spectroscopy, debris detection generated from citrus mechanical harvesting, detection of citrus fruit dropped on the ground due to disease, citrus leaf nitrogen detection, silage yield mapping, soil nutrients and grain insect detection using NIR spectroscopy.

The use of soil penetrometer resistance with soil ECa measurements may facilitate detection of changes in soil bulk density and soil water content due to compaction, natural variations in soil texture and possible effects of added organic amendments on soil salinity, soil bulk density or soil water content.

This instrument named Muon Ground Radiograph (MGR) was developed to study the fluctuation of the density in the soil that causes detection anisotropies in the arrival direction of cosmic ray muons observed in a tracker detector located underground.

They have been used in health care, drug design, environmental monitoring (in air, soil, and water), detection of biological, chemical, and toxic agents (for example, bacteria, virus, or tissue components), biotechnology, aviation, physics, oceanography, and the protection of civilian and engineering infrastructures.

Detection limits were 0.001 mg kg−1 for mineral soil and a detection limit of 0.01 0.08 mg kg−1 for LFH.

For spore detection soil and plant rhizosphere material was Shaeffer-Fulton stained [17].