Wide-angle landscape, 24mm, sharp focus, showing a stable building constructed on a tropical coral island, highlighting the geotechnical challenges of the location.

Building on Shaky Ground: Boosting Coral Sand Foundation Strength Against Explosions

Hey there! Let’s chat about something pretty wild – building stuff on coral islands. You know those gorgeous tropical spots? Turns out, they come with a unique challenge, especially when you’re thinking about big, solid structures like buildings, ports, or even airstrips. The ground beneath them, made of coral sand, is often loose and totally saturated with water. Now, add something intense like an earthquake or, in our case, an explosion, and you’ve got a recipe for disaster: liquefaction.

Why Coral Sand is Tricky

So, what’s the big deal with coral sand specifically? Well, it’s not like your typical beach sand. Coral sand particles are often irregular, they’ve got tiny holes inside (intraparticle porosity, fancy term!), and they can actually crush under pressure. This makes them behave differently than the standard silica sand most research focuses on. When a big, sudden load hits – like a blast wave – the water pressure in the sand shoots up super fast. This makes the sand lose its strength, acting more like a liquid than solid ground. Not exactly ideal for holding up a building, right? The problem is, studying this on remote islands is tough, so there’s a bit of a knowledge gap we really need to fill for safe island development.

The Blast Effect

Think about an explosion. It sends out these really quick, powerful pressure waves. Early on, folks simplified this, imagining it like a single sharp pulse. They figured out that these waves cause sand particles to rearrange, and this movement traps water, building up that dreaded pore pressure and reducing the ground’s ability to bear weight. Pretty clever stuff, and they even did experiments to prove it. Then, things got more complex – what about *multiple* explosions, maybe timed slightly apart? Turns out, delayed blasts can actually make liquefaction worse over a wider area because the pore pressure from one blast doesn’t fully go away before the next one hits. It’s like hitting the ground repeatedly while it’s still reeling. This is super relevant for big projects where multiple charges might be used.

Enter Desaturation

Okay, so liquefaction is a problem. What can we do about it? One promising idea is *desaturation*. The goal is simple: reduce the amount of water in the sand so it’s not 100% saturated. Even a little bit of air or gas in the pores can dramatically change how the sand responds to dynamic loads. Initially, people tried just pumping air in, but that could actually fracture the soil. Not good. So, smarter methods came along – chemical, biological, and the one we focused on: *electrolytic desaturation*. This method uses electrodes in the ground to split water molecules, creating tiny gas bubbles (hydrogen and oxygen) right there in the sand. It’s a much gentler way to introduce gas, and studies showed these bubbles can hang around for weeks, boosting the sand’s resistance to liquefaction significantly. It’s like giving the sand a little internal cushion.

Object photography, macro lens, 60mm, high detail, precise focusing, controlled lighting, showing tiny gas bubbles forming within saturated sand around electrode wires, representing the electrolytic desaturation process.

Our Experiment: Getting Down and Dirty

We wanted to see how this desaturation trick worked on real coral sand, specifically with a building sitting on top, under explosion conditions. So, we headed to a site in Liyang city, China. We dug a pit, filled it with coral sand brought from an island (it was loose and poorly graded, just the kind that loves to liquefy), and compacted it to a relative density of about 45%. Then, we put a scaled-down model of a 3-story reinforced concrete building on it. This model was 3D printed with glass fiber added to make it behave more like real concrete under dynamic stress.

Next up, the desaturation! We used a programmable power supply and special electrodes (like modified EKG plates, pretty neat!) to run a constant current of 2A through the saturated sand for 700 minutes. We monitored the electrical resistance, which is a good indicator of saturation. As expected, the resistance went up, telling us the water content was going down. We managed to get the saturation from a full 100% down to about 85%.

For the explosive part, we used black gunpowder, set up as six separate charges placed in a circle around the building foundation, buried 1 meter deep. We used electronic igniters to detonate them with a slight delay between each one (200-300 milliseconds). This was key to simulating that cumulative effect we talked about earlier. We kitted out the site and the building model with sensors – pore pressure sensors in the ground and acceleration sensors on each floor of the building. We also looked at settlement and bending moments in the structure.

What We Saw

Alright, the moment of truth – the explosions! What happened? First off, we saw the classic sign of liquefaction: “sand boiling.” Around the points where the charges were buried, water and sand erupted from the surface about a second after the blast. It looked exactly like boiling water, but with sand! This confirmed that liquefaction definitely occurred.

Looking at the pore pressure data, we saw that the excess pore pressure ratio (basically how much the water pressure built up compared to the initial pressure) dropped off really fast as you got further away from the explosion points. And here’s the good news: in the areas we desaturated, the maximum excess pore pressure ratio was reduced by roughly 33% compared to the fully saturated sand. That’s a significant drop!

Now, for the building’s response. The acceleration sensors showed the structure shaking, as you’d expect. The shaking was strongest at the bottom of the building and decreased as you went up, which makes sense. Interestingly, the desaturation didn’t seem to change the *acceleration* response much. However, it made a big difference to the *settlement*. The vertical settlement of the building in the desaturated sand was reduced by about 30% compared to the saturated sand. It also tilted less. So, while the shaking might feel similar, the ground beneath was much more stable, preventing the building from sinking or tilting as much. The bending moments (stress) in the building columns were highest at the bottom, also decreasing with height, and likely influenced by the ground movement.

Still life, 100mm Macro lens, high detail, precise focusing, controlled lighting, close-up of the 'sand boiling' phenomenon observed during the experiment, showing water and sand erupting from the ground surface near a sensor.

Taking it to the Computer

Field experiments are awesome, but they can be expensive and you can’t test *everything*. That’s where numerical simulations come in handy. We built a detailed computer model using some pretty sophisticated software (LS-DYNA) and material models designed for explosives (JWL), saturated soil (FHWA model, which handles pore pressure and things like particle crushing), and concrete (HJC model). This allowed us to simulate the explosion dynamics and the soil-structure interaction.

What the Numbers Tell Us

The numerical simulations backed up some of our experimental findings. They showed the same trend of excess pore water pressure decreasing rapidly with increasing distance from the blast. They also let us play around with different factors, like the initial effective stress (which is related to how much soil is sitting on top of the charge). The simulations showed that more overlying soil generally led to higher excess pore pressure, but the rate of increase slowed down with thicker layers.

We also compared our results to existing empirical formulas used to predict liquefaction. For shallow-buried charges in saturated, loose coral sand, the numerical results matched the trend predicted by Studer’s empirical model pretty well, especially regarding how liquefaction potential changes with distance. This is great because it means we might be able to use these simpler formulas for initial predictions in similar conditions.

Putting it All Together

So, what’s the big takeaway? This study combined real-world field experiments with detailed computer simulations to look at a really specific problem: buildings on coral sand foundations getting hit by explosions, and how electrolytic desaturation helps. We confirmed that delayed multiple blasts are effective at inducing liquefaction and causing significant settlement and stress on structures. Crucially, we showed that reducing the saturation of coral sand to about 85% using electrolysis *significantly* reduced the pore pressure build-up and, more importantly for the building, cut down the vertical settlement by about 30%. While it didn’t stop the shaking entirely, making the ground more stable is a huge win for preventing structural damage from excessive sinking or tilting. The numerical models helped us understand the underlying mechanisms and validated some predictive tools.

The Caveats

Of course, science is always about context. The coral sand we used has specific properties, and reshaped sand in a pit isn’t exactly the same as undisturbed ground. Explosion tests also have a bit of randomness to them. So, while our findings are super valuable, they are specific to the conditions of *this* experiment. If you’re dealing with different types of coral sand, different buildings, or different explosive loads, you’d definitely need to do targeted research.

All in all, I think we made a solid case for electrolytic desaturation as a promising way to make those beautiful, but challenging, coral island foundations safer against the big bangs. It’s a step forward in protecting structures in these vulnerable environments.

Wide-angle landscape, 24mm, sharp focus, long exposure, showing a stable building standing on a reinforced foundation near a tropical coastline at dusk, implying successful mitigation of liquefaction risks.

Source: Springer

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