{"id":27590,"date":"2018-04-30T06:57:05","date_gmt":"2018-04-30T06:57:05","guid":{"rendered":"https:\/\/blogs.agu.org\/landslideblog\/?p=27590"},"modified":"2018-04-30T06:57:05","modified_gmt":"2018-04-30T06:57:05","slug":"cracking-sliding-failures-1","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2018\/04\/30\/cracking-sliding-failures-1\/","title":{"rendered":"A surprising but important discovery on the timing of cracking-sliding failures landslides in China"},"content":{"rendered":"

A surprising but important discovery on the timing of “cracking-sliding failures” loess landslides in China<\/h4>\n

An interesting study has recently been published in the journal Natural Hazards and Earth System Science<\/a> (Li et al.<\/em> 2018 – available open access<\/a>) that looks at, amongst other things, the timing of loess landslides in China<\/a>.\u00a0 The paper presents an analysis of a dataset of what are termed as “cracking-sliding failures of loess” on the eastern Huangtu Plateau – often known as the Loess Plateau – in China.\u00a0 I haven’t heard of the term “cracking-sliding failure” previously, but in essence these are loess landslides that develop as a result of initial tensile failure, allowing sliding to develop.\u00a0 Li et al.<\/em> (2018)<\/a> point out that these landslides cause high levels of loss, noting that there have been over 1000 landslides of this type on China in the last two decades, causing an average of over 100 fatalities per annum.<\/p>\n

The authors have compiled a database of 1176 cracking-sliding failures in a part of the Loess Plateau, all of which have occurred in the last 20 years.\u00a0 They have then looked in detail at the timing of failure – one part of the analysis examines the annual cycle of landslides.\u00a0 This diagram, from the paper, presents the annual cycle of cracking-sliding failures:<\/p>\n

\"cracking-sliding

The annual cycle of cracking-sliding failures on the Loess Plateau in China. Figure from Li et al.<\/em> (2018)<\/a><\/p><\/div>\n

.<\/p>\n

In general, the annual cycle closing matches the seasonality of rainfall, as expected.\u00a0 But note the secondary peak in March and April – this is interpreted as being the result of the rise in temperatures in the spring, when the upper portion of the frozen layer starts to thaw.\u00a0 They hypothesise that this thawing process drives both frost heave and weakening of the soil through a collapse of the pore structure.<\/p>\n

Even more interesting is the time of day in which the landslides occurred:-<\/p>\n

\"cracking-sliding

The time of day in which cracking-sliding failures occurred on the Loess Plateau. Figure from Li et al.<\/em> (2018)<\/a><\/p><\/div>\n

.<\/p>\n

The data suggest that the failures occur preferentially in period between 10 pm and 5 am.\u00a0 The authors do not really explain why this should be the case, other than noting that there is a huge temperature change through the daily cycle, which drives thermal expansion and contraction, which might in turn drive weakening.\u00a0 I am not convinced by this explanation, given that most of the failures are driven by rainfall.\u00a0 Does the heaviest rainfall happen at night? But I think this daily cycle is a fascinating finding, which needs further research.<\/p>\n

Of course 10 pm to 5 am is the very worst time for landslides to occur from a human perspective.\u00a0 The combination of darkness and the likelihood of people being asleep inevitably drives high levels of loss.<\/p>\n

Reference<\/h4>\n

Li, Y., Mao, J., Xiang, X., and Mo, P. 2018 Factors influencing development of cracking\u2013sliding failures of loess across the eastern Huangtu Plateau of China<\/a>, Natural Hazards and Earth System Sciences<\/em>, 18<\/strong>, 1223-1231, https:\/\/doi.org\/10.5194\/nhess-18-1223-2018.<\/span><\/p>\n

 <\/p>\n","protected":false},"excerpt":{"rendered":"

A new paper (Li et al. 2018) in the journal Natural Hazards and Earth System Sciences makes a surprising but important discovery on the timing of “cracking-sliding failure” loess landslides in China<\/p>\n","protected":false},"author":22,"featured_media":27592,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[16,881,469,232,192,17],"class_list":["post-27590","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-uncategorized","tag-china","tag-east-asia","tag-featured","tag-loess","tag-paper","tag-research"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/27590","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=27590"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/27590\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media\/27592"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=27590"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=27590"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=27590"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}