Morphology of largeHalimeda bioherms,eastern Java sea (Indonesia): A side-scan sonar study     

Harry H. Roberts  Charles V. Phipps  Lukman L. Effendi 《Geo-Marine Letters》1987,7(1):7-14

The most extensive and thickestHalimeda bioherms reported from modern seas occur along both open and protected margins of Kalukalukuang Bank, eastern Java Sea (Indonesia). Seismic profiles suggest these features average 20 to 30 m thick (maximum 50 m) and developed over large areas by coalescence of individual mounds. Bioherm morphologies range from numerous small mounds ( 10–20 m diameter) through hay-stack features ( 100 m diameter) to broad swells. Some modern bank bioherms display surface forms that appear related to onbank flow from Makassar Strait. Upwelling of cold, nutritive water is likely responsible for unusualHalimeda productivity and large bioherm development.  相似文献   

Pattern of migration to an industrial area: a case study in Lhokseumawe,Aceh, Sumatera,Indonesia     

Effendi TN 《The Indonesian journal of geography》1979,9(37):33-44

The author attempts to identify factors influencing decisions to migrate to an industrial area of Sumatra, Indonesia. Reasons for migration, characteristics of migrants, and social assimilation at the place of destination are analyzed using data obtained in a 1978 study of 150 migrants to two subdistricts in Sumatra  相似文献   

Correction: Impact of excessive groundwater pumping on rejuvenation processes in the Bandung basin (Indonesia) as determined by hydrogeochemistry and modeling     

Taufiq  Ahmad  Hosono  Takahiro  Ide  Kiyoshi  Kagabu  Makoto  Iskandar  Irwan  Effendi  Agus J.  Hutasoit  Lambok M.  Shimada  Jun 《Hydrogeology Journal》2018,26(4):1263-1279

In the Bandung basin, Indonesia, excessive groundwater pumping caused by rapid increases in industrialization and population growth has caused subsurface environmental problems, such as excessive groundwater drawdown and land subsidence. In this study, multiple hydrogeochemical techniques and numerical modeling have been applied to evaluate the recharge processes and groundwater age (rejuvenation). Although all the groundwater in the Bandung basin is recharged at the same elevation at the periphery of the basin, the water type and residence time of the shallow and deep groundwater could be clearly differentiated. However, there was significant groundwater drawdown in all the depression areas and there is evidence of groundwater mixing between the shallow and deep groundwater. The groundwater mixing was traced from the high dichlorodifluoromethane (CFC-12) concentrations in some deep groundwater samples and by estimating the rejuvenation ratio (R) in some representative observation wells. The magnitude of CFC-12 concentration, as an indicator of young groundwater, showed a good correlation with R, determined using ¹⁴C activity in samples taken between 2008 and 2012. These correlations were confirmed with the estimation of vertical downward flux from shallower to deeper aquifers using numerical modeling. Furthermore, the change in vertical flux is affected by the change in groundwater pumping. Since the 1970s, the vertical flux increased significantly and reached approximately 15% of the total pumping amount during the 2000s, as it compensated the groundwater pumping. This study clearly revealed the processes of groundwater impact caused by excessive groundwater pumping using a combination of hydrogeochemical methods and modeling.

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