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首页> 外文期刊>Geomorphology >Forty three years of micro-erosion meter monitoring of erosion rates on shore platforms at Kaikoura Peninsula, South Island, New Zealand
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Forty three years of micro-erosion meter monitoring of erosion rates on shore platforms at Kaikoura Peninsula, South Island, New Zealand

机译:新西兰南岛凯库拉半岛海岸平台侵蚀速率的微型腐蚀仪监测长达43年

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摘要

Using micro-erosion meters (MEM) and traversing micro-erosion meters (TMEM), surface lowering rates of shore platforms on Kaikoura Peninsula, South Island, New Zealand have been measured over a total of 43 years. This record is the longest monitored network of this type. Since 1973, erosion rates have been calculated over two, two year periods 1973-1975, (n = 31) and 1993-1996, (n = 55) and at decadal scales; 1973-1993 (n = 15), 1973-2004 (n = 12), 1993-2004 (n = 46), 1993-2008 (n = 34),1993-2016, (n = 18), 1973-2016 (n = 6). After 43 years, surface lowering rates remain similar to previously published rates at an average of 0.525 to 1.181 mm. a(-1). Statistical analysis shows that erosion rates over all measurement periods are derived from the same population. Thus, short term rates derived from two years of monitoring remain indicative of decadal rates of erosion. Variations between measurement periods are best explained by the loss of the more rapidly eroding bolt sites. These losses point to the difficulty of maintaining monitoring over longer time scales. A means of statistical manipulation (previously published) allows for these losses to be accounted for in determining long term rates of platform lowering. In November 2016 a M-w 7.8 earthquake raised the Kaikoura Peninsula approximately 0.8-1 m, elevating much of the shore platforms above the tide range. This earthquake has reset the MEM record ending this long running erosion monitoring site of shore platform surface lowering. However the MEM network is now being used to monitor post-earthquake response of the uplift shore platforms and new marine terraces. (C) 2019 Published by Elsevier B.V.
机译:使用微侵蚀计(MEM)和横移微侵蚀计(TMEM),对新西兰南岛Kaikoura半岛海岸平台的表面降低率进行了总共43年的测量。该记录是此类监视时间最长的网络。自1973年以来,在1973-1975年(n = 31)和1993-1996年(n = 55)的两年时间里,以十年为单位计算侵蚀率; 1973-1993(n = 15),1973-2004(n = 12),1993-2004(n = 46),1993-2008(n = 34),1993-2016,(n = 18),1973-2016( n = 6)。 43年后,表面下降速率保持与以前公布的速率相似,平均为0.525至1.181 mm。 a(-1)。统计分析表明,所有测量期间的侵蚀率均来自同一种群。因此,从两年的监测中得出的短期比率仍然表明年代际侵蚀率。测量周期之间的变化最好用更快腐蚀的螺栓位置的损失来解释。这些损失表明难以在更长的时间范围内进行监视。统计操作的一种方法(先前已发布)允许在确定平台降低的长期速率时考虑这些损失。 2016年11月,7.8级M-w地震将Kaikoura半岛抬高了约0.8-1 m,使大部分岸台高出了潮汐范围。这次地震重置了MEM记录,结束了这个长期运行的海岸平台表面下降的侵蚀监测站点。但是,现在已经使用MEM网络来监视隆升的岸台和新的海洋阶地的地震后响应。 (C)2019由Elsevier B.V.发布

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