{"id":636,"date":"2008-06-04T08:04:00","date_gmt":"2008-06-04T08:04:00","guid":{"rendered":"http:\/\/blogs.agu.org\/landslideblog\/2008\/06\/04\/updated-tangjiashan-beichuan-dam-a-summary-of-what-we-know\/"},"modified":"2010-10-21T13:55:22","modified_gmt":"2010-10-21T17:55:22","slug":"updated-tangjiashan-beichuan-dam-a-summary-of-what-we-know","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2008\/06\/04\/updated-tangjiashan-beichuan-dam-a-summary-of-what-we-know\/","title":{"rendered":"Updated: Tangjiashan (Beichuan) dam &#8211; a summary of what we know"},"content":{"rendered":"<p>In the next 24-48 hours the water level at <span class=\"blsp-spelling-error\">Tangjiashan<\/span> should reach the spillway and flow should start.  I thought therefore that it would be useful to summarise what we know about the site:<\/p>\n<ul>\n<li>The landslide dam is 124 metres high;<\/li>\n<li>At the time that the <span class=\"blsp-spelling-corrected\">over topping<\/span> begins the lake will have a volume of about 205 million cubic metres of water (UPDATED &#8211; the volume is now estimates as 211.6 million cubic metres as at 2 pm (loca) Wednesday.  The lake level had 1.37 m to go before reaching the spillway)<\/li>\n<li>The channel that has been cut appears to be about 5 (now known to be 7  m) wide at the bed (though note that the film with the journalist in the bed suggested less than this) and about 15 m at the top.  It is 12 m deep  The bed is unlined and unprotected.  It is formed in silty materials with a few <span class=\"blsp-spelling-error\">clasts<\/span> (stones);<\/li>\n<li>Failure can occur through any of three mechanisms:<\/li>\n<ul>\n<li>The water can reach the spillway and start to flow over the dam;<\/li>\n<li>The two known seepage points (total reported flow = 10 cubic metres per second) in the dam could cause collapse;<\/li>\n<li>A landslide into the lake could trigger a wave that would <span class=\"blsp-spelling-error\">overtop<\/span> the dam.  A dangerous slope has been identified at <span class=\"blsp-spelling-error\">Xuanping<\/span> township.<\/li>\n<\/ul>\n<li>Downstream there are three further (smaller) landslide dams in the <span class=\"blsp-spelling-error\">Beichuan<\/span> area;<\/li>\n<li>The Chinese government has relocated about 250,000 people.  In total, about 1.3 million would be threatened by total collapse.<\/li>\n<\/ul>\n<div style=\"text-align: center\"><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/08_05-Tangiashan-2.jpg\"><img decoding=\"async\" style=\"margin: 0px auto 10px;text-align: center;cursor: pointer\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/08_05-Tangiashan-2.jpg\" alt=\"\" border=\"0\" \/><\/a><span style=\"font-size:85%\"><span style=\"font-family:verdana\">Reuters image of the top of the dam showing the lake and the spillway under construction<\/span><\/span><\/div>\n<p>These are the best and worst case scenarios for the dam as I see them:<br \/>Best case: water flows over the spillway and erodes it slowly.  The lake level reduces gradually over a few weeks;<br \/>Worst case: a large landslide into the lake triggers a wave that <span class=\"blsp-spelling-error\">overtops<\/span> the dam, causing complete collapse.  The entire volume of the lake is released very rapidly.  The resultant flood pools behind and then breaks through the downstream dams, creating a devastating debris flow.<\/p>\n<p>The most likely scenario at this stage is that water will flow over the spillway.  A ball park flow rate appears to be about 100 cubic metres per second when there is no rainfall.  This channel will not be able to cope with this as far as I can see, leading to rapid erosion and therefore collapse of the dam.  I suspect that most of the lake volume will be released in a few days at most.  <span class=\"blsp-spelling-corrected\">The<\/span> water is likely to pool briefly behind the landslide dams downstream, which will probably increase the size of the flood wave once released.<\/p>\n<p>Where will the water go?  I have tried to produce a quick Google Earth summary image below of the anticipated flow path (click on the image for a better view):-<\/p>\n<p><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/08_06-beichuan-flow-path-2.jpg\"><img decoding=\"async\" style=\"margin: 0px auto 10px;text-align: center;cursor: pointer\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/08_06-beichuan-flow-path-2.jpg\" alt=\"\" border=\"0\" \/><\/a><br \/>The flood is likely to be large, fast and very damaging in the mountains, but should spread at least a little and slow on the plains. We can only hope for the best.<\/p>\n<p>I am travelling to Nepal this afternoon, but will do what I can to keep this updated from there.<\/p>\n<!-- AddThis Advanced Settings generic via filter on the_content --><!-- AddThis Share Buttons generic via filter on the_content -->","protected":false},"excerpt":{"rendered":"<p>In the next 24-48 hours the water level at Tangjiashan should reach the spillway and flow should start. I thought therefore that it would be useful to summarise what we know about the site: The landslide dam is 124 metres high; At the time that the over topping begins the lake will have a volume of about 205 million cubic metres of water (UPDATED &#8211; the volume is now estimates &hellip;<!-- AddThis Advanced Settings generic via filter on wp_trim_excerpt --><!-- AddThis Share Buttons generic via filter on wp_trim_excerpt --><\/p>\n","protected":false},"author":22,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[333,16,57,23,59,15,132],"class_list":["post-636","post","type-post","status-publish","format-standard","hentry","category-uncategorized","tag-333","tag-china","tag-debris-flow","tag-earthquake","tag-flood","tag-landslide-dam","tag-sichuan"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/636","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/users\/22"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/comments?post=636"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/636\/revisions"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=636"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=636"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=636"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}