Designer Ice Cream Mix up a Batch of Ice Cream and Freeze It with an Ice Bath
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Sophie's Ice Cream Cartopens PDF File
Connect your circuits to rPower* to control them remotely from a smartphone or tablet! Alice and Bettina became friends in their university’s master’s *Sold separately. engineering program, and soon discovered that they were both TM inspired to pursue engineering by childhood toys. To help inspire the We wanna hear about all the fun you had! Contact us at: Customer Service, 1400 E. Inman Pkwy., Beloit, WI 53511 • [email protected] • 1-800-524-4263. ® For more fun, visit playmonster.com Copyright © 2016 PlayMonster LLC, Beloit, WI 53511 USA. Made in China. All rights reserved. Roominate, The creative wired next generation of innovators, Alice and Bettina designed Roominate ! building kit and Switch on Your Imagination are trademarks of PlayMonster LLC. BUILD the Ice Cream Cart and a table! 2 Bonjour! I’m Sophie, and I can’t wait to see the ice cream cart you 1 design for me! ABOUT SOPHIE Favorite Activities: Cooking, reading and learning French Favorite Foods: Chicken noodle soup, cookies and ice cream Favorite Project: I have developed the best chocolate chip cookie recipe…it’s amazing how much chemistry is in cooking! Favorite Scientist: Dorothy Hodgkin Fun Fact: I’m planning to backpack in Europe after I graduate! I Want to Be: A chemist so I can design new medicine to help people, and discover ways for everyone to have clean water and healthy food! WIRE Collect all of the You can also add a motor to make it move! Sold separately. More designs at dolls, pets and roominatetoy.com! Roominate® kits! 1 2 Actual color of pieces in your set may be dierent from those shown here. -
Ice Cream Cone Pan 2105-2087
Instructions for To Decorate Ice Cream Cone Cake You will need Wilton Icing Colors in Ivory, Golden Yellow, Rose; Tips 3, Baking & Decorating 16; Wilton Rainbow Jimmies Sprinkle Decorations. We suggest you tint all icings at one time, while the cake cools. Refrigerate icing in covered Ice Cream Cone containers until ready to use. Make 3 cups buttercream icing: Cakes • Tint 1/4 cup dark Ivory/Golden Yellow combination • Tint 1 1/4 cups light Ivory/Golden Yellow combination PLEASE READ THROUGH INSTRUCTIONS BEFORE YOU BEGIN. • Tint 1 1/2 cups rose (thin with 1 Tablespoon + 1 1/2 teaspoons light IN ADDITION, to decorate cake you will need: corn syrup) • Wilton Decorating Bags and Couplers or Parchment WITH DARK IVORY/GOLDEN YELLOW ICING Triangles • Use tip 3 and “To Make Outlines” directions to outline waffle pattern on co n e • Tips 3, 16 • Wilton Icing Colors in Ivory, Golden Yellow, Rose WITH LIGHT IVORY/GOLDEN YELLOW ICING (alternate design uses Kelly Green) • Use tip 16 and “To Make Stars” directions to cover cone • Cake Board, Fanci-Foil Wrap or serving tray WITH THINNED ROSE ICING • One 2-layer cake mix or ingredients to make favorite • Use spatula to ice fluffy bottom scoop, then top scoop layer cake recipe Immediately sprinkle scoops with rainbow jimmies. • Buttercream Icing (recipe included) • Alternate designs use Chocolate Mousse and Chocolate Buttercream Icing (recipes included) or Wilton Chocolate Ready-To-Use Decorator Icing, Wilton Candy Melts® in Light Cocoa and Pink, Wilton Rainbow Nonpareils and Rainbow Jimmies Sprinkle Decorations, Wilton Vanilla Whipped Icing Mix, chocolate chips, red gumball, favorite crisped rice cereal treat recipe, vegetable pan spray, light corn syrup Wilton Method Cake Decorating Classes Iced fluffy with thinned rose Sprinkle with icing rainbow jimmies Call: 800-942-8881 © 2003 Wilton Industries, Inc. -
Jökulhlaups in Skaftá: a Study of a Jökul- Hlaup from the Western Skaftá Cauldron in the Vatnajökull Ice Cap, Iceland
Jökulhlaups in Skaftá: A study of a jökul- hlaup from the Western Skaftá cauldron in the Vatnajökull ice cap, Iceland Bergur Einarsson, Veðurstofu Íslands Skýrsla VÍ 2009-006 Jökulhlaups in Skaftá: A study of jökul- hlaup from the Western Skaftá cauldron in the Vatnajökull ice cap, Iceland Bergur Einarsson Skýrsla Veðurstofa Íslands +354 522 60 00 VÍ 2009-006 Bústaðavegur 9 +354 522 60 06 ISSN 1670-8261 150 Reykjavík [email protected] Abstract Fast-rising jökulhlaups from the geothermal subglacial lakes below the Skaftá caul- drons in Vatnajökull emerge in the Skaftá river approximately every year with 45 jökulhlaups recorded since 1955. The accumulated volume of flood water was used to estimate the average rate of water accumulation in the subglacial lakes during the last decade as 6 Gl (6·106 m3) per month for the lake below the western cauldron and 9 Gl per month for the eastern caul- dron. Data on water accumulation and lake water composition in the western cauldron were used to estimate the power of the underlying geothermal area as ∼550 MW. For a jökulhlaup from the Western Skaftá cauldron in September 2006, the low- ering of the ice cover overlying the subglacial lake, the discharge in Skaftá and the temperature of the flood water close to the glacier margin were measured. The dis- charge from the subglacial lake during the jökulhlaup was calculated using a hypso- metric curve for the subglacial lake, estimated from the form of the surface cauldron after jökulhlaups. The maximum outflow from the lake during the jökulhlaup is esti- mated as 123 m3 s−1 while the maximum discharge of jökulhlaup water at the glacier terminus is estimated as 97 m3 s−1. -
Let's Crank Some Ice Cream
Let’s Crank Some Ice Cream! The history of ice harvesting, the ice industry, refrigeration, and making ice cream Kathi Elkins 7-29-19 OLLI: Summer 2019 Ice Storage and Ice Houses: 1780 BC --- ice house in northern Mesopotamian 1100 BC --- evidence of ice pits in China By 400 BC --- Persian engineers had mastered techniques of constructing yakhchāl to store ice harvested from nearby mountains. 300 BC --- Alexander the Great (snow pits to hold snow and ice) 200s AD --- Romans (snow shops) Cold springs, root cellars Ice Houses: Yakhchāl (this one at Yazd, Iran) is a Persian ice pit or a type of evaporative cooler. Above ground, the structure had a domed shape, but had a subterranean storage space. It was often used to store ice and food. The subterranean space coupled with the thick heat-resistant construction material insulated the storage space all year. Ice Houses: Ice houses in England/UK. Ice Houses: Croome's thatched ice house, Worcestershire, UK Ice Houses: Botany Bay Icehouse, Edisto Island, SC Ice Houses: Ice house designs usually began as an underground egg-shaped cellar. This ice house, dating from 1780s and designed by architect John Nash, was discovered in 2018 buried under London streets. In 1822, following a very mild winter, William Leftwich chartered a vessel to Norway to collect 300 tons of ice harvested from crystal-clear frozen lakes. Previous imports had been lost at sea, or melted while baffled customs officials dithered over how to tax such unique cargo. John Nash designed the Royal Pavilion at Brighton, as well as Buckingham Palace. -
ICE CREAM MAKER Instruction Manual & Recipes
ICE CREAM MAKER Instruction Manual & Recipes MODEL: AIC-100 (Capacity: 1 Quart) Congratulations on your purchase of Aroma's Ice Cream Maker. It allows you to make your own rich and creamy HOMEMADE ice cream or frozen yogurt with the flip of a switch. You can also make your own favorite, healthy and delicious sherbet, sorbet, ice and frozen drinks fast and easy with Aroma Ice Cream Maker. Enjoy your new Ice Cream Maker, it is fun and easy! Please read all instructions carefully before using this product. Published By: Aroma Housewares Company 6469 Flanders Drive San Diego, CA 92121 U.S.A. ©2003 Aroma Housewares Company IMPORTANT SAFEGUARDS Basic safety precautions should always be followed when using electrical appliances, including the following: 1. Read all Instructions before using the appliance. 2. To protect against electrical hazard, do not immerse main body-the motor base or other electrical cord in water or other liquid. 3. Close supervision is necessary when any appliance is used by or near children. 4. Unplug appliance from outlet when not in use, before putting on or taking off parts and before cleaning. 5. Avoid contacting moving parts. Keep fingers, hair, clothing, as well as spatulas and other utensils away during operation. 6. Do not operate any appliance with a damaged cord or plug or after the appliance malfunctions or is dropped or has been damaged in any manner. Return appliance to the nearest authorized service facility for examination, repair or adjustment. 7. The use of accessory attachments not recommended by the appliance manufacturer may cause hazards. -
Daisy at Home Recipe for a Small Glacier
Daisy at Home Recipe for a Small Glacier Supplies Scientific Concepts • 1 pint of chocolate swirl or Glacier: A huge, thick sheet marble ice cream. of moving ice. They are often found in mountains, • 3 of your favorite kinds of cookies. but can be found in other places, too. Washington • 1/4 cup of light-colored was half covered in a syrup (butterscotch, glacier during the Ice Age! marshmallow, etc.) • Plastic sandwich bag or similar. Glacial till: Materials, such as rocks and dirt, left • A clear bowl. behind when a glacier • A spoon. melts. Most of the soil in the Seattle area is made of glacial till. Daisy at Home Recipe for a Small Glacier Instructions 1. Crumble up the cookies and put them in the bowl. This represents dirt and rocks that will become glacial till. 2. Put two big scoops of the ice cream on top of the crumbled cookies. Glaciers begin as clean snow and ice, but they pick up dirt and rocks from the ground as they travel. So, the ice cream with its swirls represents this “dirty” glacier! 3. Slide the plastic sandwich bag over your hand. Then, slowly push down or “smoosh” the ice cream so it oozes! What do you notice? What happens to the cookie crumbles? A glacier moves in a similar way. As more snow falls on it, the added weight causes the glacier to “ooze” or “flow,” pushing the dirt in all directions. 4. To see how glaciers flow, heat up your light-colored syrup and pour it over the ice cream. -
Gas Hydrates As a Functional Foaming Agent for Viscous Food Matrices
Research Collection Doctoral Thesis Gas Hydrates as a Functional Foaming Agent for Viscous Food Matrices Author(s): Šedivá, Zuzana Publication Date: 2019 Permanent Link: https://doi.org/10.3929/ethz-b-000352862 This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms of use. ETH Library Diss. ETH No. 25820 Gas hydrates as a functional foaming agent for viscous food matrices A dissertation submitted to attain the degree of DOCTOR OF SCIENCES of ETH ZURICH (Dr. sc. ETH Zurich) presented by Zuzana Šedivá MSc in Food Science ETH Zurich born 26th May 1987 citizen of Czech Republic accepted on the recommendation of Prof. Dr. E. J. Windhab, Examiner Dr. Martin Leser, Co-Examiner Dr. Vincent Meunier, Co-Examiner 2019 Summary A novel technology for foaming viscous slurries was designed. The process involved a crystalline gas hydrate dispersion as a functional ingredient standing in the core of the technology. Gas hydrates, also known as clathrate hydrates, are solid inclusion compounds, in which gas molecules are physically entrapped in a network of cavities made up of water molecules held together by hydrogen bonds (Marinhas et al., 2007). Gas hydrates exist at moderate pressures and low temperatures and possess a high volumetric gas storage capacity. The innovative idea of replacing highly energetically demanding foaming of viscous slurries using pure gas with the gas hydrate technology emerges in the current study. Introducing a gas as a slurry in its solid clathrate form into another viscous product stream reduces the energy input otherwise needed in powerful mixing devices. -
December 23, 1903
menatn l SUBSCRIPTION PRICK. #2.00 PER TlAR. mod!| i ENTf RED AS SECOND CLAS8 MATTER 1 XLIX, Vol. I IP PAID IN ADVANCE, #1.50 1903. No. ELLSWORTH, MAINE, WEDNESDAY AFTERNOON, DECEMBER 23, f AT THE ELLSWORTH POST OF-ICE. { 51. 'aubertMcmente. LOCAL AFFAIRS George F. Hank ell; delegate to State en- TWO BIO FIRES. campment, James L. Cook; alternate, W. C. R. R, SOLD THE OLD RELIABLE Dorephus L. Fields. How Ellsworth Suffered in the Days SKW A DVKKTISEM ENTS THIS WEKK. PAID THE of Misses Annie and Helen Mitchell, ac- $2,300,000 FOR DOWN Long Ago. Tbe recent disastrous at In bankruptcy—Est Chas II White. companied by their brother Asa, have EAST ROAD. conflagration Waller H Brooks—Notice of foreclosure. Cherryfield brings to the minds of Elia- Hancock George H Waaso<i—Notice of foreclosure. gone to Massachusetts and New Hamp- County Savings Bank, worth’s oldest inhabitants two serious Han Fair A Co *s’n—Stockholders’ meeting. shire for a short visit among relatives and ONLY TWENTY PERSONS PRESENT AND First Nat’I hank—'Stockholders* meeting. conflagrations in Ellsworth’s history, one Flluworth Loan A Ass’n—Annual friends. ONLY ONE BID—PROMPTLY ACCEPTED ORGANIZED MARCH Building of which 17, 1873, I®* '»ng. occurred on Dec. 12, 1845, the Esoteric lodge will work the third de- AND FORFEIT DEPOSITED. In bankruptcy— K"t Calvin H Norris. other nine years later, on Dec. 24, 1851. has semi-annual In Kst Harvey W Hodgkins. on four candidates this An paid regular dividends amounting to *201,*11.01 bankruptcy— gree evening. -
Science Lesson Plan
How Do Glaciers Scratch And Move Rocks? Purpose: Students will model the action of a rock-filled glacier with ice cubes and learn how glaciers can make scratches in Earths surface. Text: McGraw Hill, Pg. 175 Explore Activity McGraw Hill Science Journal, Pg. 75 Resources: I have added an additional experiment that you can do in your classroom after lab to reinforce the concepts being taught this week. Learning Outcomes: Students will discuss and know how glaciers scratch and move rocks. (Homeroom Teacher) Bridge-in: Share student’s hypothesis with class: How can a block of ice help shape the Earth’s surface? Prior Knowledge: How are icebergs formed? Do you think that a glacier is able to make scratches in the Earth’s surface? If YES, then HOW? If NO, then WHY? Input from you: Review what a prediction is. What is meant by using, the word, variable(s) in an experiment? What is an observation? What do I mean when I use the term inference? (Science Facilitator) Materials: Science Notebook Science Journal Pg. 75 Paper towels Clean ice cubes Ice cubes made with sand Aluminum foil Wood scraps, large enough to scrape ice cubes against. Guided Procedure: Predict: Which ice cube do you think is more like a real glacier? Record your prediction and reasons in your journal. Using Variables: Think about how you could use the materials to test your ideas. Which ice cube will scratch a surface? Record your observations for each ice cube. Observation: Which cube will leave “rocks” behind? Place the ice cubes on a folded paper towel. -
RECIPE for MAKING LIQUID NITROGEN ICE CREAM (Serves About 18-20 Students)
RECIPE FOR MAKING LIQUID NITROGEN ICE CREAM (serves about 18-20 students) NOTE: This is NOT a regular ChemDemo activity but rather a “treat” to go along with a regular ChemDemo 1. Add 1 quart Half and Half and 1 quart Heavy Whipping Cream into a large plastic or glass salad or punch bowl. 2. Add ¾ to 1 cup of granulated sugar (1 cup is a little on the sweet side). 3. 4-5 teaspoons of vanilla. 4. Optional: 1 pound of fresh fruit or preserves (not jelly). Strawberry or peach works best. If using fresh fruit, cut into small pieces. Chocolate syrup (8 oz) works well to make chocolate ice cream. If using chocolate syrup use less sugar (½ to ¾ cup). 5. Stir the mix for 2-3 minutes to dissolve the sugar. 6. Add about 2-3 liters of liquid nitrogen slowly and in small portions into the mix and stir with a wooden spoon. Pour a little at a time and stir; then continue adding small amounts of liquid nitrogen until you have the desired consistency. One person should be stirring while another gradually pours in the LN2. Another person may be necessary to hold the container when it starts getting thick. 7. Allow any excess liquid nitrogen to boil off. 8. Serve to your audience. Enough for 20 students (half a cup each). 9. Wash equipment and enjoy. SAFETY NOTE: LN2 is extremely cold (-196°C, -321°F, 77 K)!! Spilling it on you can cause serious frost- bite burns! Pouring some on unprotected skin is actually less dangerous than on clothing in contact with skin. -
Becoming-The-Iceman.Pdf
FOREWORD Becoming the Iceman is a project inspired by Wim and Justin to show the world that anyone can adopt the ability to become an Ice- man or Icewoman. The project’s goal is to show that the ability to control the body’s temperature is not a genetic defect in Wim, but an ability that can be adopted by anyone. For many generations, we have been taught to fear the cold: “Don’t forget your jacket! You don’t want hypothermia, do you?” “Put your gloves on before you get frostbite!” Of course, these are consequences of extreme cold exposure, but with the proper understanding, anyone can learn to use the cold as a natural teacher. You may have seen Wim running around on television, barefoot in the snow or swimming in ice-cold waters. While he is doing those incredible feats, he isn’t worried about how cold it is; he is enjoying himself. Like any new tool, you must understand how it works before you can use it efficiently. This pertains to the cold as well. Wim is the epitome of what can happen if someone uses the cold to train the body. You might ask, “How can you prove that anyone can learn this ability?” We’re glad you asked… As of Fall 2009, Justin Rosales had no experience with the cold whatsoever. He was a college student attending Penn State Univer- sity. After Justin’s friend, Jarrett, showed him one of Wim’s videos on YouTube, they became exceedingly interested in understanding this ability. They wanted to see if it was possible for anyone to learn. -
Supplement of Debris Cover and the Thinning of Kennicott Glacier, Alaska: in Situ Mea- Surements, Automated Ice Cliff Delineation and Distributed Melt Estimates
Supplement of The Cryosphere, 15, 265–282, 2021 https://doi.org/10.5194/tc-15-265-2021-supplement © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Supplement of Debris cover and the thinning of Kennicott Glacier, Alaska: in situ mea- surements, automated ice cliff delineation and distributed melt estimates Leif S. Anderson et al. Correspondence to: Leif S. Anderson ([email protected]) The copyright of individual parts of the supplement might differ from the CC BY 4.0 License. Supplementary Materials S1 In situ measurements Fig. S1 Schematic of sub-debris melt rate and ice cliff backwasting rate measurements. Fig. S2 High-resolution orthoimage with medial moraines delineated. WorldView image from 13 July 2009 (catalog ID: 1020010008B20800) is shown in both panels. a) Image with medial moraines delineated and labeled. b) Image with medial moraines delineated, labeled, and with elevation contours from 2013. 69 % of debris thickness measurements are from medial moraines 5-7. A trail up the east side of the glacier allowed easy access to medial moraines 1, 2, and 3. More data is collected there than on the west side of the glacier. Note the light color debris in medial moraine 9, which is debris in excess of ~1 m thick. 1 Fig. S3 Map of the general study area with in situ measurement locations. a) Locations of sub-debris melt rate measurements. Map of the study area with contours derived from 2013. b) Locations where ice cliff backwasting was measured. The ice extents are derived from WV imagery and aerial photos.