1 00:00:09,093 --> 00:00:12,693 Speaker 1: You're listening to a podcast from News Talks be follow 2 00:00:12,773 --> 00:00:16,133 Speaker 1: this and our wide range of podcasts now on iHeartRadio. 3 00:00:16,853 --> 00:00:20,213 Speaker 2: We have been talking broadly about landslides and landslips. How 4 00:00:20,253 --> 00:00:23,053 Speaker 2: do you assess the danger? We're keeping it away specifically 5 00:00:23,372 --> 00:00:26,453 Speaker 2: from the landslip in Mount Morganui because we don't have 6 00:00:26,533 --> 00:00:30,653 Speaker 2: the details and obviously that recovery and rescue operation is underway. 7 00:00:30,813 --> 00:00:33,693 Speaker 2: But to chat further broadly about landslides and landslips, we 8 00:00:33,732 --> 00:00:36,893 Speaker 2: are joined by Andrew Stalt. He is a geo mechanical 9 00:00:36,933 --> 00:00:40,732 Speaker 2: engineer at Auckland University. Andrew, very good afternoon to you, 10 00:00:40,812 --> 00:00:41,933 Speaker 2: and thank you very much for your time. 11 00:00:42,772 --> 00:00:45,253 Speaker 3: Hi Taylor, thank you for having me Andrew. 12 00:00:45,412 --> 00:00:49,132 Speaker 4: It's Matt here as well. How are you today? Now? 13 00:00:49,132 --> 00:00:53,333 Speaker 4: How do you spot a bank or a cliff that 14 00:00:53,533 --> 00:00:56,053 Speaker 4: might be about to slip. 15 00:00:58,093 --> 00:01:00,453 Speaker 3: There's a few things, so to give it away. The 16 00:01:00,493 --> 00:01:03,133 Speaker 3: first is, well, if you look at the slope itself, 17 00:01:03,333 --> 00:01:06,253 Speaker 3: if it's step thirty five degrees, pretty hard to hike up, 18 00:01:06,893 --> 00:01:09,053 Speaker 3: that might be a slope that could business suceptible. And 19 00:01:09,093 --> 00:01:12,613 Speaker 3: it's usually soil slopes at that and you might see 20 00:01:12,613 --> 00:01:14,652 Speaker 3: a few things. You can look up at the slope 21 00:01:14,733 --> 00:01:17,892 Speaker 3: and what we call a scarp. So at the top, 22 00:01:18,053 --> 00:01:20,053 Speaker 3: if a slip is starting to happen, you might see 23 00:01:20,093 --> 00:01:22,813 Speaker 3: evidence of cracks forming at the top of the slope, 24 00:01:23,253 --> 00:01:25,413 Speaker 3: indicating that mass is going to come down and move 25 00:01:25,453 --> 00:01:28,893 Speaker 3: at you closer to the ground, closer to you know, 26 00:01:28,893 --> 00:01:31,652 Speaker 3: and where we might have houses, more flat ground, you'll 27 00:01:31,652 --> 00:01:34,932 Speaker 3: start to see the soil slumping. You might see if 28 00:01:34,932 --> 00:01:37,333 Speaker 3: you have a retaining wall it's starting to tilt more 29 00:01:37,453 --> 00:01:41,572 Speaker 3: towards well down slope. You might see cracks forming in 30 00:01:41,613 --> 00:01:44,773 Speaker 3: the ground at the toe or in your pavement, in 31 00:01:44,813 --> 00:01:48,853 Speaker 3: your your your concrete backyard. Yeah. 32 00:01:48,893 --> 00:01:52,533 Speaker 4: What role do trees play in slip Prevenchin We've been 33 00:01:52,533 --> 00:01:55,013 Speaker 4: talking about this a bit today and what are the 34 00:01:55,013 --> 00:01:57,093 Speaker 4: best trees to stop slops? 35 00:01:57,133 --> 00:02:01,293 Speaker 3: In New Zealand, you kind of have different two different 36 00:02:01,413 --> 00:02:03,453 Speaker 3: types of slope failures that you're kind of worried about. 37 00:02:03,773 --> 00:02:06,493 Speaker 3: You have the very near surfaced ones where the soil 38 00:02:06,573 --> 00:02:09,653 Speaker 3: is being eroded away or carried by water as you know, 39 00:02:09,733 --> 00:02:13,973 Speaker 3: slips along the surface, and so trees and vegetation are 40 00:02:14,013 --> 00:02:17,572 Speaker 3: actually great at helping to hold those slopes together, preventing 41 00:02:17,653 --> 00:02:20,933 Speaker 3: those what I would call a shallow failure. And so 42 00:02:21,413 --> 00:02:25,693 Speaker 3: I don't I don't know what specific trees would be 43 00:02:25,733 --> 00:02:28,493 Speaker 3: the most beneficial, but you want things with really sturdy, 44 00:02:28,573 --> 00:02:32,493 Speaker 3: strong roots. The trees will be a little bit more, 45 00:02:32,972 --> 00:02:36,893 Speaker 3: they won't be as helpful. And the more deep sleated landslides, 46 00:02:36,972 --> 00:02:40,613 Speaker 3: the ones that sometimes you see, the really deep curving 47 00:02:40,693 --> 00:02:42,692 Speaker 3: surfaces that you might see, you know, on the roadslips 48 00:02:42,693 --> 00:02:47,053 Speaker 3: when you're driving by, the roots aren't deep enough to 49 00:02:47,293 --> 00:02:52,853 Speaker 3: really interact or to help stabilize that those deep seated failures. 50 00:02:52,933 --> 00:02:57,453 Speaker 4: Yeah, and what role does a geotechnical engineer have and 51 00:02:57,933 --> 00:03:00,532 Speaker 4: this whole business across the country in terms of adentifying 52 00:03:00,653 --> 00:03:05,213 Speaker 4: slips and installing slip prevention. 53 00:03:06,933 --> 00:03:10,053 Speaker 3: Yeah, so you're geotechnical, Well, they'll look for a few things. 54 00:03:10,093 --> 00:03:11,933 Speaker 3: They'll try to figure out how strong the earth is. 55 00:03:11,972 --> 00:03:15,533 Speaker 3: So if it's soil, they'll look at its friction, its strength, 56 00:03:15,773 --> 00:03:20,053 Speaker 3: ability to hold together. They'll look at the geometry of 57 00:03:20,093 --> 00:03:22,373 Speaker 3: the failure. So if the slope is really steep, that's 58 00:03:22,373 --> 00:03:24,733 Speaker 3: just something that at least when I'm even just driving 59 00:03:24,773 --> 00:03:26,493 Speaker 3: by on the side of the road, I'll look and say, yeah, 60 00:03:26,532 --> 00:03:29,893 Speaker 3: that's a little steep, little suss And so that's when, yeah, 61 00:03:29,972 --> 00:03:34,213 Speaker 3: your geotechnical engineer will look at those issues. The other 62 00:03:34,213 --> 00:03:36,893 Speaker 3: thing they might help do is if you're looking at 63 00:03:36,933 --> 00:03:40,253 Speaker 3: retaining a slope or if you're planning on cutting a 64 00:03:40,373 --> 00:03:43,773 Speaker 3: slope on your property, talking to a geotechnical engineer will 65 00:03:43,773 --> 00:03:48,293 Speaker 3: help assess that water is a big thing that really 66 00:03:48,373 --> 00:03:50,893 Speaker 3: drives these failures. As we all know, we have these 67 00:03:50,973 --> 00:03:53,973 Speaker 3: rainfall events and then we suddenly have slips all over 68 00:03:54,013 --> 00:03:54,493 Speaker 3: the country. 69 00:03:54,573 --> 00:03:54,733 Speaker 1: Right. 70 00:03:54,933 --> 00:03:59,213 Speaker 3: Yeah, and so the water does two things. It's increasing 71 00:03:59,253 --> 00:04:02,693 Speaker 3: the load on the slope, so basically the soil weighs more. 72 00:04:03,653 --> 00:04:06,653 Speaker 3: The other aspect is that the soil partially gets the 73 00:04:06,773 --> 00:04:11,893 Speaker 3: strength from friction, and when you add more water into 74 00:04:11,933 --> 00:04:15,213 Speaker 3: the slope, it's temporarily kind of pushing those grains a 75 00:04:15,213 --> 00:04:18,853 Speaker 3: little bit apart. And so geotechnical engineers, if you look 76 00:04:18,893 --> 00:04:20,653 Speaker 3: at the side of roads, when you're driving along the 77 00:04:20,693 --> 00:04:24,133 Speaker 3: motorway and you see retaining walls, there's almost always drains 78 00:04:24,213 --> 00:04:26,373 Speaker 3: installed at the bottom of the slope or a retaining 79 00:04:26,413 --> 00:04:29,133 Speaker 3: walls just to help or leave that excess water pressure. 80 00:04:29,293 --> 00:04:32,013 Speaker 2: Makes a lot of sense. Yeah, absolutely, Andrew, We've only 81 00:04:32,013 --> 00:04:34,533 Speaker 2: got about thirty seconds left. But are there some good 82 00:04:34,573 --> 00:04:37,933 Speaker 2: places people can go if they want to find some resources, 83 00:04:37,973 --> 00:04:38,813 Speaker 2: get some more information. 84 00:04:39,933 --> 00:04:42,813 Speaker 3: Yeah, so there's an ongoing research projects where we're trying 85 00:04:42,813 --> 00:04:47,973 Speaker 3: to identify these landslide hazards. Hore Tiri Retue Penoa Sliding 86 00:04:48,053 --> 00:04:51,493 Speaker 3: Lands program also for this general so we're looking at 87 00:04:51,533 --> 00:04:53,533 Speaker 3: where these landslipes are likely to happen in the face 88 00:04:53,573 --> 00:04:59,053 Speaker 3: of climate change. Also, I recommend looking at Tokatoake. The 89 00:04:59,133 --> 00:05:02,173 Speaker 3: Natural Hazards Commission has great advice on what to look 90 00:05:02,213 --> 00:05:04,853 Speaker 3: for and then after a slope stability issue happens, what 91 00:05:04,933 --> 00:05:08,173 Speaker 3: you can maybe do to help help solve your issues. 92 00:05:08,453 --> 00:05:11,013 Speaker 2: That's brilliant. Andrew, thank you very much for your time. 93 00:05:11,053 --> 00:05:14,373 Speaker 2: Really appreciate it. That is Andrew Stok, GEO mechanics engineer 94 00:05:14,413 --> 00:05:15,973 Speaker 2: at Auckland University. 95 00:05:16,533 --> 00:05:19,173 Speaker 1: For more from news Talks at b listen live on 96 00:05:19,253 --> 00:05:22,213 Speaker 1: air or online, and keep our shows with you wherever 97 00:05:22,253 --> 00:05:24,853 Speaker 1: you go with our podcasts on iHeartRadio