![]() ![]() The first is to test which of three end-member conceptual models describing water flow (plug flow, lateral flow, bypass flow) within the Miami oolite are effective in draining large amounts of rainwater into the subsurface. ![]() This paper demonstrates how densely sampled and precisely repeated ground-penetrating radar (GPR) surveys can track fluid movement and characterize the subsurface flow regime at a field site in the Miami oolitic limestone. Even combined, these methods lack the resolution to describe how or where the water is moving on the centimeter to meter scales. Traditional investigations rely on interpolation between point measurements (rock samples and borehole tests), and/or low resolution two-dimensional (2-D) geophysical methods (e.g., surface or borehole resistivity and electromagnetic techniques). It is essentially impossible to characterize drainage using standard hydrogeological methods. Subsequent to the rapid infiltration, little is known regarding the nature of water flow paths and rates in this complex environment. Water from heavy summer storms that ponds on the surface to depths of several centimeters disappears within a fraction of an hour. For example, in large parts of urban Miami the vadose zone is characterized by oolitic carbonates, where laterally varying small-scale stratigraphy and crosscutting dissolution features control transport pathways. Three-dimensional connectivity creates preferential flow paths allowing large volumes of water, nutrients, and contaminants to rapidly bypass the less permeable bulk rock volume. Rainfall/water table response times, well drawdown tests, slug tests, pump tests, and tracer experiments exhibit surprisingly high hydraulic conductivities, orders of magnitude higher than those derived from measurements on rock plugs taken from both outcrops and cores. Subsurface fluid flow in carbonates is often controlled by a highly heterogeneous hydraulic conductivity field resulting from the interplay of small-scale sedimentary structure, diagenetic alteration, and fracturing. High-precision time-lapse GPR imaging can therefore be used to noninvasively characterize natural drainage inside the vadose zone ranging from transient loading to seasonal variation. Comparing 3-D surveys acquired after wet summer and dry winter conditions shows good GPR event correspondence, but also time shifts up to 20 ns caused by the change of overall water content within the vadose zone. On a seasonal time frame, redistribution involves the entire rock volume. Average lateral propagation measured over a 28-hour period was of the order of 0.1 m/h. ![]() At the same time, some of the water migrates laterally into the host rock guided by stratigraphic unit boundaries. Hourly repeated 3-D imaging of a dissolution sink in response to surface infiltration shows how the wetting front propagates at a rate of 0.6–1.2 m/h traversing the 5-m-thick vadose zone within hours. Two-dimensional (2-D) GPR time-lapse surveying at a 3-min interval before, during, and after rainfall shows how buried sand-filled dissolution sinks efficiently drain the bulk of the rainwater. A new rotary laser-positioned ground-penetrating radar (GPR) system enables centimeter-precise and rapid acquisition of time-lapse surveys in the field. Once the water enters the ground, little is known about the flow paths in the oolitic rock. ![]() The vadose zone of the Miami limestone is capable of draining several centimeters of rainfall within a fraction of an hour. ![]()
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Yes, that's partially because I'm spending less time on my phone, but it's also because my thoughts aren't moving in a hundred different directions before I go to sleep. I (delusionally) tell myself "I'm going to go to bed early tonight!" almost every night, but since I got the Loftie clock, I actually do. It's a slow way to ease in to my morning rather than being inundated with information first thing. Now, I wake up to the soothing sound of birds chirping out of the Loftie clock before selecting one of the many guided meditation, soundbath, or breathwork practices to do. I was spending up to an hour each morning and night checking social media, emails, and texts. I didn't realize how long it was taking me to get out of bed and to fall asleep till I completely removed the option of passively scrolling Instagram in bed. $165 at Credit: Courtesy It saves me hours of time. 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My urge to reach for my iPhone and spend (too much) time scrolling social media was totally ruining my sleep till I started using the Loftie Clock ( Loftie, $165). I've been meditating and doing yoga daily since I was 16, but that doesn't mean I'm zen from the moment I wake up till I crawl back in to bed. ![]() ![]() ![]() The game is played on a smaller field and the pitchers throw under hand. Soft ball is a sport similar to baseball, but the ball is larger and softer. I hope that these quotes provide some inspiration for you the next time you need a little boost ! Cat Osterman – The Left-Handed, 4-Time All American Pitcher.Welcome to my blog post about inspirational soft ball quotes ! As a soft ball player myself, I know how important it is to have motivational words to help get you through tough times on the field.Lisa Fernandez – The Record-Setting Fastpitch Player with an Olympic Record.Dot Richardson – A Veteran Pitcher with an Olympic Reputation.In 2010 Finch retired from softball she was inducted into the ASA/USA Softball Hall of Fame in 2016. Usually, the shortstop is the most athletic player on the field and must have various skills such as explosive agility, arm strength & range, glove skills & hand-eye coordination, and an excellent understanding of what is happening on the field. The hardest position to play in softball is the shortstop. What is the hardest position in softball? Jennie Finch’s underhand fastball pitch comes in at around 68 mph. An average changeup for this age is somewhere around the 50-60 mph mark. A pitcher throwing 75 mph is well above average for this age, and their fastball is at a high school caliber. How fast should a 13 year old pitch?Ī typical fastball from this age group is anywhere from 55 mph (on the low side) to 75 mph. Who is the oldest college softball player?ģ2-year-old Michele Westmorland, returning to college, picks right back up with softball, after some serious prep. Three people Jennie would love to have dinner with are Jesus, Oprah, and her husband, Casey. Jennie wears sweat pants 99% of the time. Jennie’s dream vacation is to go to Australia. The Chicago Bandits stadium address is 27 Jennie Finch Way. He then tied the glove tightly to create a ball out of it. He was the one to shout “play ball” when the boxing glove was first used to play the game in 1887 at the Farragut Boat Club in Chicago. George Hancock, when he founded the game, was a reporter with the Chicago Board of Trade. Who is the best softball pitcher of all time? Jennie Finch is more than just an Olympic softball player she is a leader who inspires many lives every day due to her confidence, selflessness and moral strength despite all the setbacks she has overcame in her life and on her road to success. In the end she, as a devout Christian, made peace with her fame because she felt she could use it to be a role model to young women and to help grow the game of softball. She struggled with the notoriety, which in a team sport is sometimes a problem. team for the 2008 Games in Beijing as one of the most well-known softball players in the world. ![]() softball team to the gold medal at the 2004 Olympic Games in Athens, and she returned to the U.S. Are you looking for the answer to the question: What Was Jennie Finch Known For? We have gathered for you the most accurate and comprehensive information that will fully answer the question: What Was Jennie Finch Known For?Īmerican softball player Jennie Finch helped propel the U.S. ![]() ![]() ![]()
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