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AEOLIAN SAND TRANSPORT HIGH FREQUENCY LONG PERIOD CALIBRATION

机译:风沙运输高频率长时间校准

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Studies have been carried out, from April 1999 to April 2000, in Tróia (SW Portugal)rnin order to identify aeolian sand transport inhibitor factors during one year, aiming properrncalibration of known models. Photogrammetry, beach/dune system surveys and a high frequencyrnvertical sensor array were used to estimate aeolian sand transport. Calculated transport for allrndirections was 2.02 m3m-1year-1 with resultant of 1.58 m3m-1year-1 landwards – double ofrnmeasured value for 1958-99 time interval and up to three times measured survey values at sensorrnarray location, averaging 0.44 m3m-1year-1 for entire profile dune distance. Results show the needrnof local high frequency sensor calibration for better inhibitor factors understanding, improvingrnestimated/measured transport ratio. Expected self-recovery rates of the studied dune systemrn(1 m3 m-1) extend from 10 months to 3.3 years. However, sediment availability and single pointrnsensor readings are, still, non-controlled factors.
机译:为了确定已知模型的正确性,从1999年4月至2000年4月,在特洛亚(葡萄牙西南部)进行了研究,以识别风沙输送抑制剂因素。摄影测量法,海滩/沙丘系统调查和高频垂直传感器阵列用于估算风沙的运输。计算得出的所有方向的运输量为2.02 m3m-1year-1,向陆地的运输量为1.58 m3m-1year-1-1958-99时间间隔的测量值的两倍,在传感器阵列位置的测量值最高为三倍,平均为0.44 m3m-1year-1对于整个轮廓沙丘距离。结果表明需要对局部高频传感器进行校准,以更好地了解抑制因子,从而改善重新评估/测量的转运比。沙丘系统的预期自我恢复率(1 m3 m-1)从10个月延长至3.3年。但是,沉积物的有效性和单点传感器的读数仍然是不受控制的因素。

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