首页> 外文期刊>Natural Hazards >The September 8-9, 1998 Rain-Triggered Flood Events at Motozintla, Chiapas, Mexico
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The September 8-9, 1998 Rain-Triggered Flood Events at Motozintla, Chiapas, Mexico

机译:1998年9月8日至9日在墨西哥恰帕斯州Motozintla引发的洪水引发的洪水事件

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In September 1998 tropical storm "Earl" swept southern Mexico, producing intense rainfall in the states of Oaxaca and Chiapas. Among the most devastated cities was Motozintla, located in the drainage basin of the Allende, La Mina and Xelaju Grande Rivers. The rainfall from the tropical storm totaled 175 mm on September 8 and 130 mm on September 9, duplicating in two days the average monthly precipitation in the region. Numerous landslides occurred in the vicinity of Motozintla, depositing large volumes of material into the Xelajii Grande stream. Much of this sediment was subsequently remobilized, yielding debris flows, hyperconcentrated flows, and sediment-laden flows that inundated most sections of Motozintla city. The flows covered an approximatearea of 3.15 km~2 with a minimum volume of 4.4 x 10~6 m~3 of sediment. Communication of Motozintla with the rest of the Chiapas State was interrupted for about a month, as was the supply of potable water, food, electricity, and fuel. The geologic recordaround Motozintla indicates that the Xelajii Grande River has been a pathway for similar large floods during the last 6000 years. The oldest deposit yielded a radiocarbon age of 5320 ± 100 ~(14)C years. B.P. At least two historic floods have occurred during the last 100 years, a time period defined by a stratigraphically distinct tephra of 1902. Frequency analysis of the historical record of daily rainfall in the Motozintla area suggests that events like that of September, 1998, have a recurrence interval of about 25 years. After the catastrophic flows of 1998, the mitigation measures by Municipal Authorities were made without regard to geological and environmental factors, or to taking into consideration the flow magnitude and appropriate hazard-mitigation techniques, with the result that Motozintla remains at serious risk for future floods. Unfortunately, prior to the publication of this study, in early October 2005, Motozintla was seriously damaged again by intense rain provoked by Hurricane Stan.
机译:1998年9月,热带风暴“厄尔”席卷墨西哥南部,在瓦哈卡州和恰帕斯州产生大量降雨。受灾最严重的城市是位于阿连德,拉米纳河和谢拉茹格兰德河流域的摩托辛特拉。热带风暴的降雨量在9月8日达到175毫米,在9月9日达到130毫米,在两天内使该地区的月平均降雨量增加了一倍。 Motozintla附近发生了许多滑坡,将大量物质沉积到Xelajii Grande流中。随后,大部分沉积物被清除,产生了泥石流,高浓度泥沙流和充满泥沙的泥沙流,淹没了Motozintla市的大部分地区。流量覆盖约3.15 km〜2的区域,最小体积为4.4 x 10〜6 m〜3的沉积物。 Motozintla与恰帕斯州其他地区的通讯中断了大约一个月,饮用水,食物,电力和燃料的供应也中断了。 Motozintla周围的地质记录表明,在过去的6000年中,Xelajii Grande河一直是类似大洪水的通道。最古老的矿床的放射性碳年龄为5320±100〜(14)C年。 B.P.在过去的100年中,至少发生了两次历史性洪灾,这一时期由1902年地层上的特非拉定义。对Motozintla地区日降雨历史记录的频率分析表明,像1998年9月这样的事件有一次复发间隔约25年。在1998年灾难性洪水之后,市政当局采取的缓解措施既没有考虑地质和环境因素,也没有考虑流量的大小和适当的减灾技术,结果Motozintla仍然面临着未来洪水的严重风险。不幸的是,在这项研究发表之前,2005年10月上旬,斯坦飓风引发的强烈降雨再次严重破坏了Motozintla。

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