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Wash load is similar to a suspended load, but wash load sediment never interacts with the bed load. All of the sediment in the wash load stays suspended in the water throughout the channel (this concept has been debated). Wash load refers to a river's ability to move sediment through a channel. Hans Albert Einstein described wash load as "if the sediment is added to the upstream end of a concrete channel and the channel is swept clean, and the sediment has not left any trace in the channel".

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  • ウォッシュロード (ja)
  • Wash load (en)
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  • ウォッシュロード(英語:wash load)は、よりも細かい粒径の土砂で構成されている流砂である。流速が遅くなってもなかなか沈殿しないため、ひとたび流水中に取り込まれれば、長い距離を流下しやすい。 ウォッシュロードの粒径範囲は、0.1 - 0.2mm以下程度である。 * d>0.1 - 0.2mmの粒子は、掃流力の増加に対応して、掃流状態から浮遊状態へ遷移する。しかし、その遷移は急激ではなく、掃流砂と浮遊砂が共存する輸送形式をもって、河床を構成する砂礫となる。 * d<0.1 - 0.2mmの粒子は、摩擦速度が掃流限界を超える付近で、浮遊砂への移行が急激に生じる。主として浮遊形式で輸送され、移動河床中にはほとんど存在しえず、ウォッシュロードとなる。 (ja)
  • Wash load is similar to a suspended load, but wash load sediment never interacts with the bed load. All of the sediment in the wash load stays suspended in the water throughout the channel (this concept has been debated). Wash load refers to a river's ability to move sediment through a channel. Hans Albert Einstein described wash load as "if the sediment is added to the upstream end of a concrete channel and the channel is swept clean, and the sediment has not left any trace in the channel". (en)
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  • Wash load is similar to a suspended load, but wash load sediment never interacts with the bed load. All of the sediment in the wash load stays suspended in the water throughout the channel (this concept has been debated). Wash load refers to a river's ability to move sediment through a channel. Hans Albert Einstein described wash load as "if the sediment is added to the upstream end of a concrete channel and the channel is swept clean, and the sediment has not left any trace in the channel". The sediments in the wash load are generally smaller than .0625 mm. What determines the wash load is the relationship between the size of the bed load and the size of the particles that never settle in the "fine sediment load" or wash load. (en)
  • ウォッシュロード(英語:wash load)は、よりも細かい粒径の土砂で構成されている流砂である。流速が遅くなってもなかなか沈殿しないため、ひとたび流水中に取り込まれれば、長い距離を流下しやすい。 ウォッシュロードの粒径範囲は、0.1 - 0.2mm以下程度である。 * d>0.1 - 0.2mmの粒子は、掃流力の増加に対応して、掃流状態から浮遊状態へ遷移する。しかし、その遷移は急激ではなく、掃流砂と浮遊砂が共存する輸送形式をもって、河床を構成する砂礫となる。 * d<0.1 - 0.2mmの粒子は、摩擦速度が掃流限界を超える付近で、浮遊砂への移行が急激に生じる。主として浮遊形式で輸送され、移動河床中にはほとんど存在しえず、ウォッシュロードとなる。 (ja)
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