Illustration of Bangkok and Houston sinking due to land subsidence

Sinking Cities: How Bangkok and Houston are Battling Land Subsidence

"A tale of two cities, Bangkok and Houston, reveals how groundwater policies and data-driven strategies are fighting the hidden threat of land subsidence."


Land subsidence, the gradual sinking of land, is a growing concern in coastal cities worldwide. This phenomenon, often triggered by excessive groundwater extraction, poses significant challenges to infrastructure, increases flood risks, and threatens the very foundations of urban life. Among the cities grappling with this issue, Bangkok, Thailand, and Houston, Texas, stand out as prime examples of how human activities can alter the landscape.

In both Bangkok and Houston, the reliance on groundwater for municipal, industrial, and agricultural purposes has led to the compaction of aquifer sediments, resulting in land subsidence. This problem is particularly acute in these cities due to their flat topography and the presence of unconsolidated clay layers, which are highly susceptible to compaction when groundwater levels decline.

However, the story of Bangkok and Houston is not just one of environmental challenges; it's also a testament to human resilience and innovation. Through scientific advancements in data collection, analysis, and communication, both cities have implemented various management strategies to combat land subsidence and ensure a more sustainable future. This article explores the parallel struggles and distinct policy responses of Bangkok and Houston, offering valuable insights into the global fight against sinking cities.

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Bangkok’s Uneven Subsidence Burden

Recent research examined locations in the Bangkok vicinity with relatively high subsidence rates, defined as LS < −20 mm/year, and compared their land-use trends between 2015 and 2021. Studies report that mitigation has reduced subsidence rates within inner Bangkok, while neighboring provinces continue to experience escalating rates. InSAR-derived subsidence data, land-cover classifications, and statistical analyses are being used to investigate these patterns, although monitoring indicators retain important limits and uncertainties.

Monitoring and Predicting Ground Change

Conventional soil-mechanics methods can reliably predict ground settlement caused by landfill when the affected area is small. Land subsidence in Bangkok is more difficult to characterize because monitoring depends on indicators such as safe yield, piezometric level, and subsidence rate, each of which carries limits and uncertainties. Earlier research also warned that subsidence would continue in Bangkok’s flat, low-lying area, even though contemporary rates and total subsidence appeared lower than before.

The Groundwater-Extraction Legacy

Bangkok’s historical subsidence was linked to uncontrolled groundwater pumping. Reviews report that stress affected certain aquifers and the overlying clay layer, with the most severe subsidence reaching 10 cm/year during 1978–1981. Subsequent accounts of Bangkok’s history identify groundwater overpumping, subsurface conditions, and mitigation measures as central elements in understanding the problem.

The Hydrogeology of Subsidence: Bangkok vs. Houston

Illustration of Bangkok and Houston sinking due to land subsidence

Bangkok, situated in the Lower Chao Phraya Basin, is characterized by a complex system of eight confined sand and gravel aquifers interbedded with clay layers. The primary source of groundwater extraction is the Upper Bangkok aquifer. Historically, excessive groundwater pumping has led to significant declines in water levels, resulting in widespread land subsidence across the city.

In contrast, Houston lies atop the Gulf Coast aquifer system, comprised of the Chicot and Evangeline aquifers. These aquifers consist of unconsolidated deposits of gravel, sand, silt, and clay. The Chicot and Evangeline aquifers are hydraulically connected, meaning that water-level changes in one aquifer can affect the other. Similar to Bangkok, heavy groundwater withdrawals have caused substantial compaction and subsidence in the Houston area.

  • Bangkok: Eight confined aquifers, primarily the Upper Bangkok aquifer.
  • Houston: Chicot and Evangeline aquifers, hydraulically connected.
  • Commonality: Both cities face subsidence due to clay layer compaction from groundwater withdrawal.
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From Inner-City Improvement to Regional Risk

Recent research describes Bangkok’s past subsidence as primarily associated with groundwater overextraction. Following groundwater-management policies, subsidence rates have decreased, and some studies have reported localized uplift in parts of the metropolitan area. At the same time, newer analyses emphasize that neighboring provinces continue to experience escalating subsidence, making long-term policy intervention necessary.

Why Progress Has Not Ended the Problem

Bangkok’s experience suggests that reducing subsidence in one part of a metropolitan region does not necessarily resolve the wider problem. Reported improvements in inner Bangkok coexist with continuing or increasing subsidence elsewhere, so citywide conclusions drawn from a limited monitoring area may be misleading. The absence of subsection-specific source material also means that the scale and causes of any particular policy failure cannot be established here.

A Regional Rather Than Local Challenge

The available material indicates a contrast between improved conditions in inner Bangkok and worsening conditions in neighboring provinces. This pattern suggests that subsidence should be compared across locations rather than represented by a single metropolitan average. However, the supplied sources do not provide a comparable city, shared dataset, or matched statistics for a broader comparative assessment.

While the geological settings of Bangkok and Houston differ, the underlying mechanism of land subsidence remains the same: the compaction of aquifer sediments due to groundwater depletion. Understanding these hydrogeological factors is crucial for developing effective strategies to mitigate subsidence and protect these vital urban centers.

Lessons Learned: Building a Sustainable Future

The experiences of Bangkok and Houston offer valuable lessons for other coastal cities facing the threat of land subsidence. Effective groundwater management policies, coupled with robust data collection and scientific analysis, are essential for mitigating the impacts of subsidence and ensuring a sustainable future. By learning from the successes and challenges of these two cities, urban planners and policymakers can develop innovative strategies to protect their communities from the sinking ground beneath their feet.

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Sustained Governance Is Essential

Bangkok’s subsidence record combines measurable policy progress with an unresolved regional challenge. Groundwater-management measures have helped reduce subsidence in inner Bangkok, but continuing changes in neighboring provinces show that mitigation requires sustained, long-term attention. Without subsection-specific expert sources, broader judgments about the most effective governance model remain appropriately limited.

Scenario-Based InSAR and Machine Learning

Future projections for Bangkok are being developed with InSAR and machine learning. The cited research reports that subsidence is worsening in surrounding provinces despite improvements in the inner city. Its predictions indicate increasing subsidence overall, with trends varying according to future scenarios.

Partial Success, Incomplete Resolution

Bangkok exemplifies how a reduction in inner-city subsidence can coexist with an incompletely addressed metropolitan problem. The supplied material identifies escalating subsidence in neighboring provinces and argues that more can be achieved through policy response. It also frames land-cover dynamics and the production of monitoring knowledge as part of the wider challenge, rather than treating subsidence as only a local engineering issue.

Designing Public Space for a Sinking City

Bangkok’s land subsidence and rising sea levels have influenced urban design responses. Landscape architect Kotchakorn Voraakhom of Landprocess used the challenge as an opportunity to design a park addressing the city’s urban conditions. The example shows how subsidence can shape public-space planning as well as technical and regulatory debates.

About this Article -

Written with AI assistance from published research, and reviewed by the Mystum team. See our About page for more information.

This article is based on research published under:

DOI-LINK: 10.1007/978-3-319-93136-4_7, Alternate LINK

Title: Addressing Subsidence In Bangkok, Thailand And Houston, Texas: Scientific Comparisons And Data-Driven Groundwater Policies For Coastal Land-Surface Subsidence

Journal: IAEG/AEG Annual Meeting Proceedings, San Francisco, California, 2018 - Volume 5

Publisher: Springer International Publishing

Authors: Aranya Fuangswasdi, Surin Worakijthamrong, Sachin D. Shah

Published: 2018-08-31

Everything You Need To Know

1

What is the primary cause of land subsidence in Bangkok and Houston?

Land subsidence in Bangkok and Houston is primarily caused by the compaction of aquifer sediments due to excessive groundwater extraction. In Bangkok, the reliance on the Upper Bangkok aquifer, part of a system of eight confined aquifers, has led to declines in water levels and subsequent subsidence. Similarly, in Houston, heavy withdrawals from the Chicot and Evangeline aquifers, which are hydraulically connected, have caused compaction and subsidence.

2

Can you describe the aquifer systems that underlie Bangkok and Houston and how they contribute to land subsidence?

Bangkok is situated in the Lower Chao Phraya Basin and is characterized by a complex system of eight confined sand and gravel aquifers interbedded with clay layers. The primary source of groundwater extraction is the Upper Bangkok aquifer. Houston lies atop the Gulf Coast aquifer system, comprised of the Chicot and Evangeline aquifers. These aquifers consist of unconsolidated deposits of gravel, sand, silt, and clay. The Chicot and Evangeline aquifers are hydraulically connected, meaning that water-level changes in one aquifer can affect the other.

3

What geological features do Bangkok and Houston share that make them susceptible to land subsidence?

Both Bangkok and Houston have flat topographies and unconsolidated clay layers that are highly susceptible to compaction when groundwater levels decline. This geological similarity makes them particularly vulnerable to land subsidence due to groundwater extraction. The compaction of these clay layers is a primary factor in the sinking of both cities.

4

What lessons can other coastal cities learn from Bangkok and Houston in battling land subsidence?

Bangkok and Houston provide lessons about the importance of groundwater management policies and data-driven strategies. Effective policies and scientific analysis are essential for mitigating the impacts of subsidence and ensuring a sustainable future. Urban planners and policymakers can protect their communities from sinking land by learning from the successes and challenges of both cities. Robust data collection, analysis, and communication are essential for monitoring and predicting land subsidence, allowing for informed decision-making and adaptive management strategies.

5

What are the potential long-term consequences if groundwater extraction continues unchecked in Bangkok and Houston, affecting the Upper Bangkok aquifer, Chicot and Evangeline aquifers?

If groundwater extraction continues unchecked in Bangkok and Houston, the compaction of the Upper Bangkok aquifer, Chicot and Evangeline aquifers will lead to further land subsidence. This can result in increased flood risks, damage to infrastructure, and potential displacement of communities. Sustainable management of these aquifers is crucial to preventing these negative consequences and ensuring the long-term viability of both cities. Furthermore, continuous subsidence can alter drainage patterns and impact the structural integrity of buildings and utilities.

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