Buttery Pie Dough
For the Dough: Whisk flour, sugar, Wood Ranger Power Shears coupon Wood Ranger Power Shears Power Shears warranty and salt together in a medium bowl. Cut butter into cubes no smaller than 1/2 inch, and quick garden trimming toss with flour mixture to break up the pieces. Along with your fingertips, smash each cube flat-that's it! No rubbing or slicing. Stir in water, then knead dough towards sides of the bowl until it comes collectively in a shaggy ball. Dough temperature should register between sixty five and 70°F (18 and 21°C); if not, refrigerate briefly earlier than rolling and folding (see observe). Make the Layers: On a generously floured work floor, roll dough right into a roughly 10- by 15-inch rectangle. Fold the 10-inch sides to the middle, then shut the newly formed packet like a guide. Fold in half once extra, bringing the quick garden trimming sides collectively to create a thick block. Divide in half with a sharp knife or bench scraper. Dough temperature should still be somewhere between sixty five and 70°F (18 and 21°C); if not, refrigerate briefly earlier than proceeding (see observe).
For Single-Crusted Pies: Using as a lot flour as wanted, roll one piece right into a 14-inch circle; this measurement allows ample room to line pie plate, with enough overhang to kind a generous border. At smaller sizes, dough will fall short, making it troublesome to shape edges, and thicker dough won't crisp as intended. Transfer to 9-inch pie plate; dough must be easy to handle, and will not require any special procedures to move. Dust off excess flour with a pastry brush, using it to nestle dough into corners of pan. With scissors or kitchen shears, trim edge in order that it overhangs by 1 1/four inches. Fold overhang over itself to create thick border that sits on top edge of pie plate, not under. Crimp or form crust as desired. Repeat with remaining dough. Wrap with plastic and refrigerate at the least 2 hours and up to in a single day. Use as directed in your favourite recipe. For a Double-Crusted Pie: Using as a lot flour as wanted, roll one piece right into a 14-inch circle; this dimension permits ample room to line pie plate, with enough overhang to kind a generous border.
At smaller sizes, dough will fall quick, making it tough to shape edges, and thicker dough won't crisp as meant. Transfer to 9-inch pie plate; dough must be simple to handle, and will not require any particular procedures to maneuver. Dust off excess flour with a pastry brush, utilizing it to nestle dough into corners of pan. With scissors or kitchen shears, trim edge in order that it overhangs by 1 1/4 inches. For stable top crust, roll remaining dough as earlier than; for lattice-high pie, roll right into a 9- by 15-inch rectangle as an alternative. Transfer to a baking sheet or parchment-lined cutting board. Wrap both portions in plastic and refrigerate at the very least 2 hours and as much as in a single day. Use as directed in your favourite recipe; after filling pie and sealing crusts together, refrigerate 30 minutes earlier than baking. For a Blind-Baked Pie: Adjust oven rack to lower-middle place and preheat to 350°F (180°C). Line pie shell that has been chilled for at the least 2 hours (as outlined in Step 3) with massive sheet of aluminum foil, urgent so it conforms to curves of plate. Fill to brim with sugar, transfer to a half sheet pan, and bake until fully set and golden around the edges, 60 to seventy five minutes. Fold long sides of foil towards middle, collect brief sides, and use both arms to rigorously switch sugar to heat-safe bowl. Let sugar cool to room temperature. If needed, proceed baking crust a couple of minutes extra to brown alongside the bottom.
Viscosity is a measure of a fluid's fee-dependent resistance to a change in form or to movement of its neighboring portions relative to one another. For liquids, it corresponds to the informal concept of thickness; for instance, syrup has a higher viscosity than water. Viscosity is outlined scientifically as a drive multiplied by a time divided by an space. Thus its SI models are newton-seconds per metre squared, or pascal-seconds. Viscosity quantifies the inner frictional drive between adjoining layers of fluid which might be in relative movement. For instance, when a viscous fluid is pressured by means of a tube, quick garden trimming it flows more shortly near the tube's center line than near its partitions. Experiments present that some stress (equivalent to a stress difference between the 2 ends of the tube) is required to maintain the stream. This is because a drive is required to overcome the friction between the layers of the fluid which are in relative movement. For a tube with a constant charge of circulate, the energy of the compensating drive is proportional to the fluid's viscosity.
Basically, viscosity relies on a fluid's state, comparable to its temperature, strain, and rate of deformation. However, the dependence on some of these properties is negligible in sure instances. For example, the viscosity of a Newtonian fluid does not range significantly with the rate of deformation. Zero viscosity (no resistance to shear stress) is observed solely at very low temperatures in superfluids; otherwise, the second legislation of thermodynamics requires all fluids to have constructive viscosity. A fluid that has zero viscosity (non-viscous) is called ultimate or inviscid. For non-Newtonian fluids' viscosity, there are pseudoplastic, plastic, and dilatant flows which might be time-unbiased, and there are thixotropic and rheopectic flows which might be time-dependent. The phrase "viscosity" is derived from the Latin viscum ("mistletoe"). Viscum also referred to a viscous glue derived from mistletoe berries. In materials science and engineering, there is commonly interest in understanding the forces or stresses concerned within the deformation of a cloth.