Abstract

Changing seasonal precipitation patterns prompted by climate change are likely causing increasing degradation of adobe architecture in the American Southwest. This deterioration includes surface erosion and catastrophic collapse. This study examines the impact of changing rainfall patterns on untreated adobe walls to understand how damage occurs and anticipate future impacts. To complete the study, we constructed 20 adobe test walls. Using a portable rain simulator, each wall was subjected to two rainfall experiments: high-intensity rainfall simulations (rain intensity variable) and low-intensity rainfall simulations (rain event number variable). Wall-degradation metrics (material loss, volume loss, affected surface area, and cavity depth) were calculated for each wall using pre- and post-simulation LiDAR scans. Internal wall moisture was also measured with embedded volumetric water content sensors. In the high-intensity experiment, the lines of best-fit for material loss and affected surface area show that surface erosion increases with rain intensity, while cavity depth remains consistent. Linear models and post-hoc tests indicate material loss and affected surface area is significantly different for each high-intensity rainfall treatment. Furthermore, the interior of each wall remained relatively dry demonstrating that rain intensity is not a strong predictor of interior wall moisture. In the low-intensity rainfall experiment, the rainfall simulations yielded statistically similar erosion and interior wall moisture results. Greater infiltration occurred under low-intensity long-duration rain conditions, while greater surficial damage occurred under high-intensity rain conditions. In conclusion, changing weather regimes are bringing more intense rainfall events to the arid American Southwest. This study suggests that more frequent high intensity rain events will cause increasing damage to adobe walls. Resource managers will need to adapt current management strategies to account for this change.

Highlights

  • Over the last decade, cultural resource managers working for the United States National Park Service (NPS) have noted increasing damage to earthen architecture from rainfall

  • High‐intensity rainfall experiment Degradation metrics demonstrated that significantly different material loss (%) and affected surface area resulted from each high-intensity treatment (Tables 6, 7, Fig. 6a, b)

  • The lines of best-fit for material loss and affected surface area showed that erosion of the adobe walls increased with rain intensity, at an increasing rate of change (Fig. 7)

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Summary

Introduction

Cultural resource managers working for the United States National Park Service (NPS) have noted increasing damage to earthen architecture from rainfall. Rainwater from storm events has caused erosion, material loss, and even catastrophic collapse of adobe architecture [1]. Tumacácori National Historical Park (NHP), near Tucson, Arizona, has suffered. Hart et al Herit Sci (2021) 9:143 four wall collapses since 2010. This damage appears to happen when rain penetrates the existing protective lime shelter and saturates underlying adobe, causing structural failure. The collapses at Tumacácori occurred during long-duration storm events in both winter and summer. The summer storm events included short periods of high-intensity rainfall

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