Rosses AC NewsLast Saturday a number of club athletes took part in the Newmills 10k where the advantage of the fairly flat course was negated by a very strong headwind during the first half of the race.Ciaran McGonagle continued his strong running this year and finished a great 2nd place in a time of 34:55 behind Ivan Toner from Letterkenny pushing him all the way to the line. Noel Diver and Kevin McGee pushed each other well over the course to finish 6th and 7th respectively with Michael Logue 12th.Aisling Diver ran a great race to finish 3rd lady in the senior women’s race.Good luck to Patrick Marry who is travelling to Jordanstown this weekend to compete in the Ulster Juveniles Even Ages.This weekend all attention turns to the October 27th, Bank Holiday Monday, which will see the running of the Dublin Marathon, on the streets and parks of the capital city. Over the years, many Rosses athletes have participated in this prestigious event.This year, the club will be represented by a number of people who have been training diligently over the past few months. Good luck to all!!!Some upcoming events are: Sunday 2nd November – Donegal Senior – Stranorlar. 9th November 12pm – Ulster Juvenile Unven Ages & Novice – Killinkere, Co. Cavan. Sunday 16th November – Remembrance 10k in Finn Valley.Sportshall Athletics will start in the gym at RCS, Dungloe after the Halloween break on Monday 3rd November at 6.45 pm for children born 2007 and older.Cross country training continues for all adults in Mullaghderg every Wednesday and Friday at 6. Club captain Michael Mc Elroy in charge. Senior Ladies training with coach Helen Mc Cready in Mullaghderg.ATHLETICS NEWS: ROSSES AC ATHLETE CIARAN MCGONAGLE CONTINUES HIS FINE FORM AT NEWSMILLS 10K was last modified: October 21st, 2014 by Mark ForkerShare this:Click to share on Facebook (Opens in new window)Click to share on Twitter (Opens in new window)Click to share on LinkedIn (Opens in new window)Click to share on Reddit (Opens in new window)Click to share on Pocket (Opens in new window)Click to share on Telegram (Opens in new window)Click to share on WhatsApp (Opens in new window)Click to share on Skype (Opens in new window)Click to print (Opens in new window)Tags:athleticsNoticesROSSES ACSport
Share Facebook Twitter Google + LinkedIn Pinterest Registration is now open for the Ohio Ecological Food and Farm Association’s (OEFFA) 37th annual conference. Pre-conference intensives will be held on Friday, February 12 and the two-day conference will take place Saturday, February 13 and Sunday, February 14, 2016 at the Granville Middle and High schools in Granville, Ohio (Licking County).As the state’s largest sustainable food and farm conference, more than 1,200 attendees from across Ohio and the U.S. will come together to enjoy keynote sessions with Lindsey Lusher Shute and John Ikerd; nearly 100 educational workshops; three pre-conference intensives; a trade show; locally-sourced and organic from-scratch meals, and more.“This conference is about working with nature, rather than trying to control it,” said OEFFA Program Director Renee Hunt. “Sustainable agriculture is not only a path for growing right by nature, but for doing right by our communities, public health, and our economy, as well.”
I like to tell people I’m a recovering academic. The truth is, though, that I haven’t left physics behind. That would be impossible since I’ve been making a career in the world of building science. So today I’m going to delve into that subset of building science called building physics as we take a look at the physics of water in porous materials. You’ll also learn about the fourth state of water, the one that’s not liquid, not solid, and not vapor.But fear not! I’m going to do all this with a lot of images, and I won’t include a single equation (although there’s a link to one if you’re brave enough to look).The polar nature of the water moleculeLet’s begin with the water molecule. One oxygen, two hydrogens, bonded together covalently. That means each hydrogen shares its one electron with the oxygen atom and both atoms get to complete their outer shells by doing so.[Image credit: Wikimedia Commons]As it turns out, the oxygen atom pulls on that shared electron from each hydrogen atom more strongly than the hydrogens do, so the oxygen side of the molecule is slightly negative. The hydrogen ends are thus slightly positive. Because the water molecule is bent (as opposed to linear, with the hydrogens on opposite sides of the oxygen), the molecule is polar. It has a negative end and a positive end. The positive charge is concentrated in two areas near the hydrogen atoms, as you can see in the illustration at left.[Image credit: Wikimedia Commons]When you put a bunch of water molecules together, the polarity of the individual molecules causes them to attract each other. Like charges repel and unlike charges attract. As you see above, each water molecule can form weak bonds, called hydrogen bonds, with four other water molecules.One consequence of water’s polarity is that it is a liquid at higher temperatures than similar molecules. Carbon dioxide, for example, is a linear, nonpolar molecule and becomes a gas at about -71° F (-57° C). If water were like carbon dioxide, the oceans would not be here. Mountains would have no snow. And I wouldn’t be writing this because we humans would not exist, at least not in the form we have now.The polarity of water molecules means that when you put it in contact with another material, what happens depends on which attraction is stronger: water for itself or water for the other material. When the water is more strongly attracted to itself, as you see on the left side of the diagram at left, we call the other material hydrophobic, or water fearing. When the water is more strongly attracted to the other material than to itself, we say that material is hydrophilic, or water-loving.When the source is liquid waterNow it’s time to recall the Second Law of Thermodynamics: Water moves from wet to dry areas.[Image credit: Stone Initiatives & Materials Testing Group]If a porous material has one end sitting in water, the pores, or capillaries, will begin filling with water. The movement of water through capillaries depends on how hydrophilic, or wettable, a surface is and on how small the capillary is. The smaller the capillary, the higher the water can rise in it, as you see in the illustration at left.The photo at the top of the article illustrates perfectly how water can move from the ground into the porous concrete and concrete block. It’s not uncommon for moisture problems in attics to originate with a wet foundation.The photo of bricks below shows the capillary rise of water over time. After a bit more than an hour, the water is three-quarters of the way up the brick.[Image credit: Wikimedia Commons]How high can the water rise? I said at the beginning I was going to do this article without equations, so I’ll just tell you that there is one you can use to calculate the height a column of water can rise in a capillary. It depends directly on how wettable the surface is and inversely on the radius of the capillary, the density of the water, and the acceleration due to gravity. (If you want to see the equation, go to the Wikipedia page on capillary action and look for the section titled Height of a meniscus.)Since trees move moisture from the ground to the leaves using capillary action, the photo below might give you an idea of how high water can rise.[Image credit: Energy Vanguard](If you look closely, you might see me standing at the base of the tree. And if you do see me there, I’ll congratulate you on your imagination.)When the source is water vaporLiquid is easy. Things start getting fun when we take a look at what happens when water vapor interacts with porous materials. If you have such a material (drywall, wood, concrete, cellulose…) with humid air on one side, water vapor will find its way into the pores. If the material is hydrophilic, water vapor will start sticking to it.And then we start using a new word. When the surface pulls water out of the air like this, we call it hygroscopic. The material is hygroscopic, and we also say that it has hygroscopic water on the surface.[Image credit: Building Science Corporation]Another word you need to know here is “adsorbed.” Those monolayers of water that stick to the surface are the fourth state of water. Here’s why.When that first monolayer of water molecules begins sticking to the surface, it does so with gusto. Remember, we’re talking about hygroscopic materials that can pull water vapor from the surrounding space. They really like each other!The second monolayer is also attracted strongly…but not as strongly as the first monolayer. Since the second monolayer is attracted to the surface through the monolayer of water that’s already there, the attraction is muted a bit. Likewise with the third, fourth, and fifth monolayers.[Image credit: Building Science Corporation (with modification by Energy Vanguard)]The diagram at left gives you a picture of that weakening attraction. The first monolayer is complete when the relative humidity rises to 10%. The relative humidity then has to rise to 50% before the second monolayer is complete. As the relative humidity keeps rising, the monolayers keep increasing and hit five by the time you get to 100%.That attraction can be put in terms of energy. Recall that the energy absorbed or emitted when water boils or condenses is called the latent heat of vaporization. When water vapor adsorbs onto a surface (or breaks free of that adsorption), there’s a latent heat of adsorption involved. According to Professor Chris Timusk, the heat of adsorption for the first monolayer is 3700 kJ/kg. For the second, it’s 2972 kJ/kg. At the fifth monolayer, the heat of adsorption is 2500 kJ/kg, which is equal to the heat of vaporization for liquid water.What that means is that the adsorbed water really is different from the other three states. It’s obviously not vapor. It’s not ice either. It’s most similar to liquid water, but it’s not as free to move as liquid because it’s bound more strongly to the surface than it is to the surrounding water molecules. Only when you get more than five monolayers do you see it beginning to act like liquid water.The three transport modesNow we’re ready to talk about how water moves through porous materials. The three transport modes are:Vapor diffusionSurface diffusionCapillary flowVapor diffusion carries water vapor through the material in the vapor state. It doesn’t stick to any of the surfaces it encounters. It just floats on through in the empty space of the pores. Not much water gets through like that.Surface diffusion moves more water than vapor diffusion. This happens because of that attraction I discussed earlier. Since the first monolayer is attracted the most strongly, it’s energetically favorable for a molecule in the second monolayer to move down to the first layer if it can, as shown below.[Image credit: Building Science Corporation (with modification by Energy Vanguard)]Likewise, molecules from the third monolayer want to move down to the second, the fourth to the third, and so on. In that fashion, water can move through a porous material via surface diffusion.But things really open up when the capillaries start filling up. Once a pore is completely full, water can move more rapidly through the porous material. That’s capillary flow.Sorption isothermsNow we can put all this together and understand what’s going on in these geeky things called sorption isotherms. The graph below, taken from Professor Timusk’s doctoral thesis, is a good example.[Image credit: Professor Chris Timusk]First, let me point out that there are three curves here: two for different densities of wood and one for clay brick. Each one shows the moisture content in the material as a function of the relative humidity of the surrounding air.Notice that each curve exhibits the same pattern: a rapid rise, a flattening out, and then another rapid rise. Recalling the explanations above for adsorption and the three types of moisture transport, what do you think is happening in those regions? See if you can figure it out before going on to the next paragraph.[Image credit: Graham van der Wielen on Flickr.com]To distract your cheating eyes from “accidentally” reading the answer first, I’ll let you look at this picture of aliens drinking beer. Now think!Well, first off, the curves show surface diffusion and capillary flow. We know capillary flow starts at higher relative humidities, so the initial rise and the flattened out part are where surface diffusion is happening. But why does the initial rise flatten out so quickly?Recall that the first monolayer feels the strongest attraction for the surface. It gets filled at about 10% relative humidity. The flat part of the curve is mostly filling the second monolayer plus a bit more in wood and significantly more in brick.When the curves shoot up again, capillary flow has kicked in (see graph below). Now the moisture content can increase rapidly with increasing relative humidity. And here’s where we can see something really interesting about the difference between materials.[Image credit: Professor Chris Timusk]Notice that capillary flow doesn’t start in the brick until the relative humidity is much higher than in the two types of wood. Hmmm. What could cause the capillaries not to fill up at lower relative humidity like it does in wood? Why of course. It’s because they’re bigger!Another important thing to know about sorption isotherms is that the curves you see above are for a specific temperature. As you raise or lower the temperature, the curves shift. Why? Because the amount of moisture a material can hold at a give relative humidity depends on how warm or cool it is.Warmer materials cannot hold as much moisture because there’s enough heat there to dry them out. Cooler materials hold more moisture. In fact, Bill Rose calls this the Fundamental Rule of Material Wetness: Warm materials tend to be dryer and cool materials tend to be wetter.And now you can look at sorption isotherms and understand what they’re telling you about materials… without being a scientist or academic, practicing or in recovery.SourcesThe main source I used for this article was chapter 3 of Professor Chris Timusk’s doctoral thesis (pdf). Most of the rest came from Dr. Joseph Lstiburek’s presentations on building science fundamentals and hygrothermal analysis, Wikipedia, and Bill Rose’s book, Water in Buildings. Allison Bailes of Decatur, Georgia, is a speaker, writer, energy consultant, RESNET-certified trainer, and the author of the Energy Vanguard Blog. Check out his in-depth course, Mastering Building Science at Heatspring Learning Institute, and follow him on Twitter at @EnergyVanguard. RELATED ARTICLESVapor Retarders and Vapor BarriersWhen Sunshine Drives Moisture Into Walls The History of Peeling Paint, Insulation, and Vapor BarriersAre Dew-Point Calculations Really Necessary?Questions and Answers About Air Barriers Q&A: Is a capillary break between the footing and foundation wall really necessary?
PayPal, the payments unit of eBay, just dropped a cool $800 million on Braintree, a smaller rival. We hope it’s not done.As we noted, Braintree will help PayPal boost its appeal to app developers, who have been frustrated with its older software and cumbersome customer-service operations.But PayPal needs more pieces to really win the battle as e-commerce takes over the physical world.I think one of those might just be Foursquare, the maker of a popular location check-in app.Checking In To RetailBraintree brought something special to PayPal: a foothold in apps that capture your credit card once and store it for future transactions. When you call a car with Uber and walk out at your destination without having to hand over your credit card, that particular bit of magic is handled by Braintree.But PayPal has another big battle in mobile payments ahead of it—and that’s in signing up local stores to take PayPal, too.It recently revamped its mobile app to emphasize local shopping and discounts. It’s easy to order a meal to go at a local restaurant and bill it to your PayPal account, for example.The challenge, though, is persuading consumers to install the PayPal app and pop it open when they’re on the move. Sure, there are coupons and other offers, but it’s hard to see those providing enough value to persuade busy users to change their routines, when there are dozens of apps fighting for their attention.Here’s PayPal Beacon, a shopper detector for stores.PayPal is also hoping to persuade merchants to install a piece of hardware called Beacon, which uses Bluetooth to identify when shoppers are nearby and let them automatically check into a store or restaurant, readying them to pay with PayPal just by saying their name.I’m skeptical of the Beacon strategy. Small businesses operate in cramped environs, and while Beacon promises to be low-maintenance, even the spare wall plug it requires might be a scarce commodity in some stores.Foursquare On The MoneyThis problem could be easily circumvented, because what Beacon does with hardware, Foursquare already does with software.You may have heard of Foursquare’s eponymous app, which people use to broadcast their location to friends. But you may be less familiar with Foursquare’s near-ubiquitous presence within other apps. When you tag an Instagram photo at a location, for example, the photo-sharing service uses Foursquare’s database of locations to tag the image.Foursquare CEO Dennis Crowley recently showed ReadWrite a detailed map of downtown San Francisco, with irregular polygons drawn around buildings. Those polygons represent a map built by the 4.5 billion check-ins Foursquare has logged to date, and that map is incredibly detailed, showing the outlines of a coffee shop within a mall.That’s the same fine-grained detail that PayPal CEO David Marcus recently told ReadWrite he wants to capture with Beacon. But Foursquare is doing it by amassing stores of data across a host of connected apps, not requiring merchants to install a proprietary piece of hardware and consumers to download the PayPal app.What Foursquare Offers PayPalBuying Foursquare would do four things for PayPal:It would give PayPal a large, user-updated database of local businesses to which it could market its payment services.It would give PayPal another product to sell those businesses besides payments—Foursquare’s still-nascent but fast-growing advertising business, where it places ads within the Foursquare app.It would boost PayPal’s appeal to mobile-app developers, by giving them another resource, Foursquare’s location database, to incorporate within their own apps.It would add teams of experienced mobile developers in New York and San Francisco—markets where it’s famously difficult to recruit talent.When you consider how PayPal is trying to expand its business, from Web-based e-commerce to app-driven local and mobile payments, a deal to buy Foursquare makes more and more sense.As to why Foursquare might sell: It’s time. The company had to borrow $41 million earlier this year instead of raising a round of equity, because its investors could not agree on how to value its brand-new advertising business. It’s been named a possible acquisition target by everyone from Google and Yahoo to Microsoft and Apple.Compared to those buyers, though, PayPal seems like it might be a more benevolent owner, less likely to squash Foursquare by integrating it into existing maps and commerce services. Foursquare considered offering payments services early in its life, but decided to avoid the cost and complexity—so while there’s good strategic fit, there’s relatively little overlap. And PayPal’s Marcus, an entrepreneur who sold a mobile-payments startup to PayPal before becoming an executive there, seems to want to leave the startups he buys alone as much as possible, rather than ruin them by integrating them too quickly.So get out that wallet, Marcus. You’ve got some shopping to do. owen thomas Tags:#acquisitions#David Marcus#Dennis Crowley#Foursquare#Location#Location-Based Services#Mobile Payments#online payments#PayPal What it Takes to Build a Highly Secure FinTech … Why IoT Apps are Eating Device Interfaces The Rise and Rise of Mobile Payment Technology Role of Mobile App Analytics In-App Engagement Related Posts