Abstract

The physical properties of soil can affect the stability of construction. In particular, soil swelling potential (a term which includes swelling/shrinking) is often overlooked as a natural hazard. Similar to risk assessment for other hazards, assessing risk for soil swelling can be defined as the product of the probability of the hazard and the value of property subjected to the hazard. This research utilizes past engineering and geological assessments of soil swelling potential, along with economic data from the U.S. Census, to assess the risk for soil swelling at the census-block level in Louisiana, a U.S. state with a relatively dense population that is vulnerable to expansive soils. Results suggest that the coastal parts of the state face the highest risk, particularly in the areas of greater population concentrations, but that all developed parts of the state have some risk. The annual historical property loss, per capita property loss, and per building property loss are all concentrated in southeastern Louisiana and extreme southwestern Louisiana, but the concentration of wealth in cities increases the historical property loss in most of the urban areas. Projections of loss by 2050 show a similar pattern, but with increased per building loss in and around a swath of cities across southwestern and south-central Louisiana. These results may assist engineers, architects, and developers as they strive to enhance the resilience of buildings and infrastructure to the multitude of environmental hazards in Louisiana.

Highlights

  • Soil that tends to swell or shrink as moisture content changes is known as expansive soil

  • Given the wide range of cost estimates and the lack of recent analysis, the purpose of this research is to introduce a more elaborate, transparent, updated, data-intensive method of calculating the risk associated with expansive soils in Louisiana, a U.S state with relatively dense population that is vulnerable to the effects of expansive soils

  • Historical expansive soil swelling potential ranges from 3.5 in northwestern and central Louisiana census blocks to 58.0 percent in both Cameron Parish in the extreme coastal southwest and in some census blocks to the west of New Orleans in Lafourche, St

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Summary

Introduction

Soil that tends to swell or shrink as moisture content changes is known as expansive soil. No matter which mechanism of movement occurs, swelling or shrinking, the hazard is known as “expansive soil” (Holtz and Hart, 1978). Expansive soils represent a separate process of soil movement from subsidence, and the two are generally not associated with each other. Scientific, soil swelling measurements and characterization date back for over a half century, when Seed et al (1962) evaluated the utility of the plasticity index [“liquid limit” percentage minus “plastic limit” percentage (Coleman and Douglas 2008)] for such purposes, but the plasticity index was later shown to be impractical in humid environments (Jones 2012). A new instrument was developed recently (Hobbs et al, 2014) and tested (Hobbs et al, 2019) for measuring shrinkage of clays

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