Abstract

Porosity is a fundamental characteristic of naturally occurring sand-textured soils, commonly referred to as natural sands, found in a wide range of landscapes, from beaches to dune fields. As a primary determinant of the density and permeability of sediments, it represents a pivotal element in geophysical studies involving basin modeling and the optical dating of sand deposits formed in areas subjected to erosion like coasts and deltas. It is also of interest for geoaccoustics and geochemical research on sediment transport and water diffusion properties of these deposits, as well as for agricultural and ecological investigations on the germination of light-sensitive seeds and the photochemical transformation of substances (e.g., pesticides) that may be present in these soils. Despite the importance of these applications, however, the remote estimation of porosity and the quantification of its effects on the light penetration profiles of natural sands remain elusive tasks. In this work, we tackle one of the major obstacles in this interdisciplinary area of research, namely the relative scarcity of experimental information due to technical constraints associated with traditional laboratory procedures. More specifically, we systematically examine the impact of porosity variations on the reflectance and transmittance of natural sands (in the 400 to 1000 nm region of the light spectrum) through controlled in silico experiments supported by measured data. Our findings are expected to strengthen the knowledge basis required for advances in this area and contribute to the development of technologies aimed at the effective monitoring and prediction of environmentally triggered changes affecting these soils.

Highlights

  • Soils are mostly composed of mineral particles of weathered rock immersed in a medium.[1]

  • Our findings suggest that advances in the remote estimation of sand deposits’ porosity will require sensors with a high degree of sensitivity

  • We note that previous works[7,17] have indicated that the permeability of sand deposits may be correlated with grain size and sphericity in addition to porosity

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Summary

Introduction

Soils are mostly composed of mineral particles (grains) of weathered rock immersed in a medium (e.g., air and/or water).[1]. When it comes to the remote estimation of porosity and the quantification of its effects on the light penetration profiles of natural sands, there is still a long way to go This may be largely attributed to the relative scarcity of experimental investigations on the putative dependence of these soils’ spectral responses on their porosity.[19,20] In order to achieve tangible advances in this area, we believe that it is necessary to examine this dependence more closely. Our findings highlight radiometric trends that need to be taken into account in the development of technologies aimed at the correct interpretation of variations in the spectral signatures of natural sands and at the reliable estimation of their porosity and light penetration profiles These technologies, in turn, will enable researchers to make inroads into the applications mentioned earlier, notably those associated with the effective monitoring and prediction of environmentally triggered changes in natural sand deposits.

In Silico Experimental Framework
Results and Discussion
Light Reflection Experiments
Light Transmission Experiments
Practical Issues
Conclusion and Future Work
Full Text
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