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Simulation of acid water movement in canals 总被引:1,自引:0,他引:1
An attempt to tackle the problem of the propagation of acid water in canals is described, and a mathematical model to simulate the acid water movement is developed, in which the jurbanite equilibrium is found to prevail. The processes of settling owing to sedimentation, precipitation and redissolution have been considered in the modelling. Data available from Tan Thanh, in the Plain of Reeds of the Mekong Delta in Viet Nam, are used as a case study. 相似文献
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Lopatin A. V. Golovachev I. V. Serdyuk N. V. Maschenko E. N. Vislobokova I. A. Dac Le Xuan Phuong Pham Mai Parkhaev P. Yu. Syromyatnikova E. V. 《Doklady Earth Sciences》2022,504(2):372-379
Doklady Earth Sciences - Speleological, geological and paleontological characteristics of the Lang Trang cave in northern Vietnam are presented. Primates Gigantopithecus blacki von Koenigswald,... 相似文献
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DUAN Zhuang FU Yangang LI Chunji ZHAO Shaorui GAO Mingbo GAO Jilei JIN Lijie LI Siyuan NGO Dac Xuan 《《地质学报》英文版》2021,95(5):1771-1774
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Vuong Van Bui Daidu Fan Dac Ve Nguyen Dinh Lan Tran Duc Thanh Tran Van Long Hoang Thi Hong Hanh Nguyen 《中国海洋大学学报(英文版)》2018,17(6):1272-1280
Coastal erosion has become a worldwide concern, typically in the densely populated Asian mega-river deltas. Severe coastal erosion in the southern Red River Delta(RRD) has been intensively studied. Coastal morphological change in the northern RRD was examined in detail through DEM(Digital Elevation Model) analysis based on time series of bathymetrical maps(1965–2004) and Landsat images(1975–2015) in this study. The results show that the northern RRD is featured by rapid coastal accretion in the past few decades, although suspended sediment flux has dropped by roughly 60% after the completeness of Hoa Binh Dam(HBD) in 1988 and relative sea level rose at 1.9 mm yr~(-1). However, accretion at the outer part of subtidal shoals and platforms was observed to slow down quickly or even turned into erosion in the last two decades. The resuspended sediments from the erosion zone can be transported landward to replenish the inner coastal zone, keeping the latter accretion in the near future to compensate for the sediment discharge decrease from the river. However, this lag effect should be terminated soon if other adverse effects go worse, e.g., damming rivers, sea-level rising, strengthening storms, land reclamation and other poor-designed coastal engineering. Coastal planners and managers should pay full attention to these changes. 相似文献
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