{"id":1268,"date":"2018-05-23T23:23:38","date_gmt":"2018-05-23T14:23:38","guid":{"rendered":"http:\/\/jsece.or.jp\/en\/?page_id=1268"},"modified":"2018-05-24T10:37:57","modified_gmt":"2018-05-24T01:37:57","slug":"336_1","status":"publish","type":"page","link":"https:\/\/jsece.or.jp\/en\/journal\/shinsabo\/no336\/336_1\/","title":{"rendered":"\u7530\u6751\u3089\uff1a\u516d\u7532\u5c71\u7cfb\u306b\u304a\u3051\u308b\u5c71\u5730\u6cb3\u5ddd\u306e\u6d6e\u904a\u7802\u306e\u8a08\u6e2c\u3068\u7279\u6027"},"content":{"rendered":"<h2 style=\"text-align: center;\">Measurement and characteristics of mountain stream wash loads in the Rokko Mountains<\/h2>\n<p style=\"text-align: center;\">Keiji TAMURA, Yasukazu KOSUGE, Taro UCHIDA,\u00a0Yoko NAGATA, Ken&#8217;ichirou KOSUGI, Takahisa MIZUYAMA<\/p>\n<h4>Abstract<\/h4>\n<p align=\"left\">pressed as a relationship between the product of the average gradient in the basin, D, and the area of the basin, A. It is expected that the relationship will depend on the geology of every region. 2) The current mechanisms for the generation and loss of wash loads in the mountain streams of the Rokko Mountains are thought to be based on the discharge of wash load components in riverbed sediment when stream water rises and the capture of these components when the water recedes. 3) When the environments that generate sediment in the basins change and the bare land ratio ra increases, \u03b1 changes by orders of magnitude. 4) When slope failure and sediment discharge occur, the bare land ratio ra increases. However, when a riverbed gravel wash load capture mechanism is held, \u03b1 does not increase. Conversely, it is predicted that when the wash load floating capture mechanisms are saturated, \u03b1 increases.<\/p>\n<h4>Key words<\/h4>\n<p>mountain stream, wash load, turbidity, riverbed sediment, Rokko Mountains<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Measurement and characteristics of mountain stream wash loads in the Rokko Mountains Keiji TAMURA, Yasukazu KOSUGE, Taro UCHIDA,\u00a0Yoko NAGATA, Ken&#8217;ichirou KOSUGI, Takahisa MIZUYAMA Abstract pressed as a relationship between the product of the average gradient in the basin, D, and the area of the basin, A. It is expected that the relationship will depend on the geology of every region. 2) The current mechanisms for the generation and loss of wash loads in the mountain streams of the Rokko Mountains are thought to be based on the discharge of wash load components in riverbed sediment when stream water rises and the capture of these components when the water recedes. 3) [&hellip;]<\/p>\n","protected":false},"author":3,"featured_media":0,"parent":1250,"menu_order":65,"comment_status":"closed","ping_status":"closed","template":"page-single-column.php","meta":{"footnotes":"","_wp_rev_ctl_limit":""},"class_list":["post-1268","page","type-page","status-publish","hentry","wpautop"],"_links":{"self":[{"href":"https:\/\/jsece.or.jp\/en\/wp-json\/wp\/v2\/pages\/1268","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/jsece.or.jp\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/jsece.or.jp\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/jsece.or.jp\/en\/wp-json\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/jsece.or.jp\/en\/wp-json\/wp\/v2\/comments?post=1268"}],"version-history":[{"count":0,"href":"https:\/\/jsece.or.jp\/en\/wp-json\/wp\/v2\/pages\/1268\/revisions"}],"up":[{"embeddable":true,"href":"https:\/\/jsece.or.jp\/en\/wp-json\/wp\/v2\/pages\/1250"}],"wp:attachment":[{"href":"https:\/\/jsece.or.jp\/en\/wp-json\/wp\/v2\/media?parent=1268"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}