Abstract

This study was carried out to assess land subsidence due to excessive groundwater abstraction in the northern region of Semarang City by integrating the application of both numerical models and geodetic measurements, particularly those based on the synthetic aperture radar interferometry (InSAR) technique. Since 1695, alluvial deposits caused by sedimentations have accumulated in the northern part of Semarang City, in turn resulting in changes in the coastline and land use up to the present. Commencing in 1900, excessive groundwater withdrawal from deep wells in the northern section of Semarang City has exacerbated natural compaction and aggravated the problem of land subsidence. In the current study, a groundwater model equivalent to the hydrogeological system in this area was developed using MODFLOW to simulate the hydromechanical coupling of groundwater flow and land subsidence. The numerical computation was performed starting with the steady-state flow model from the period of 1970 to 1990, followed by the model of transient flow and land subsidence from the period of 1990 to 2010. Our models were calibrated with deformation data from field measurements collected from various sources (e.g., leveling, GPS, and InSAR) for simulation of land subsidence, as well as with the hydraulic heads from observation wells for simulation of groundwater flow. Comparison of the results of our numerical calculations with recorded observations led to low RMSEs, yet high R2 values, mathematically indicating that the simulation outcomes are in good agreement with monitoring data. The findings in the present study also revealed that land subsidence arising from groundwater pumping poses a serious threat to the northern part of Semarang City. Two groundwater management measures are proposed and the future development of land subsidence is accordingly projected until 2050. Our study shows quantitatively that the greatest land subsidence occurs in Genuk District, with a magnitude of 36.8 mm/year. However, if the suggested groundwater management can be implemented, the rate and affected area of land subsidence can be reduced by up to 59% and 76%, respectively.

Highlights

  • Land subsidence refers to a gradual or sudden vertical deformation of the ground surface, which is usually economically and socially detrimental since it often inevitably leads to structural damages to buildings and public infrastructure, as well as expands the flood inundation area [1,2,3]

  • The northern part of Semarang City that is formed by alluvial deposits is prone to land subsidence, which has been exacerbated by over-drafting groundwater from deep wells in recent decades

  • To quantitatively analyze and model this problem, a systematic investigation of land subsidence caused by excessive groundwater abstraction was carried out in the current study using MODFLOW’s flow and subsidence packages integrated with the recorded data obtained from groundwater level observation, leveling, GPS, and Interferometric Synthetic Aperture Radar (InSAR)

Read more

Summary

Introduction

Land subsidence refers to a gradual or sudden vertical deformation of the ground surface, which is usually economically and socially detrimental since it often inevitably leads to structural damages to buildings and public infrastructure, as well as expands the flood inundation area [1,2,3]. Natural compaction and excessive groundwater enon there and has been monitored using different geodetic measurements, including are the main causes of land subsidence in Semarang City [43,45], which haslevbeen taking eling, GPS, satellite images [40,41,42,43,44]. Our model was verified by monitoring data ofmodeling crustal deformation obtained of land subsidence caused by groundwater occurs the northern of from leveling, GPS, and Sentinel-1. The effectiveness of was the performed proposed based regulatory was quantitatively groundwater management measures on our policies well-validated numerical evaluated in terms of reductions in the affected area of land subsidence in spatial and model. Evaluated in terms of reductions in the affected area of land subsidence in spatial and temporal scales

Focus of Study Area
Geological Setting
Leveling and GPS Survey for Land Subsidence Monitoring
Land Deformation Mapping
Groundwater andand
Groundwater and Geotechnical Subsidence Equation
13. Itin can be seen values arethat close to the and observed values depicted
Groundwater and Land Subsidence in the Past
Future Projection of Land Subsidence
Findings
Conclusions
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call