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What else can I help you with?
Who was anti temperance in the 1800s?
the anti-temperence leaders were called "wets"
How does water affect mass wasting processes?
I believe It changes the affect on the earth's surface, for an example: Dry sand grains are bound mainly by friction with one another. Small amounts of water increase the cohesion among sand grains. Saturation reduces friction and causes the sand to flow.
What type of Berber carpet is best?
There are lots of good carpet cleaners on the market, and they will all say pat or scrub lightly. What they don't tell you is to never pour the cleanser directly onto the carpet. That wets the carpet backing and the dyes on that will wick up through the carpet fiber. And you'll never get rid of that stain!
What are the best strategies to potty and house train a 2-month-old pup and a 3-year-old boy at the same time?
For your sanity, do both at different times. Keep lots of rags and a spray bottle full of cleaner on hand for the messes. For the boy: I would suggest a "potty training boot camp" where everyone including the dog leaves the house for 1 full day. Block off the kitchen and spend the day in there with him. Have him wear a short shirt and underware only. Fill him up with salty/sugary snacks and lots of fluids (sweet kinds to keep him drinking) so he will pee all day. Have a portable potty in the kitchen and practice "potty runs" so he gets the idea. Each time he wets or messes his underwear, have him watch you clean up the mess and make sure you have a look of disgust on your face - he needs to know that it is wrong to mess his underware. By the end of the day, he will get the basic idea and you can move the kiddie toilet to the bathroom and eventually take it away so he goes in the toilet. The rest is up to you. I don't have a dog, but friends who have tell me that the dog needs a punishment when he goes in the house. Something involving rubbing his nose in the pee/poo when he does it. Then putting him outside for awhile. The dog will learn quicker than your boy. Good luck! A 3 year old should be able to go potty on their own (with the odd accident.) For some reason some children are afraid of the toilet or "departing with a piece of themselves into the toilet bowl." For peeing, get your husband or boyfriend to go into the bathroom and pee into the toilet and then your son (make a game of it) and let your son flush the toilet (big deal for little kids.) Boys are notorious for playing hard and being too lazy to get up and go into the bathroom so, when small they can pee or poo themselves much to the mothers annoyance. Make a chart on the fridge and everytime he goes to the bathroom give him a big gold star (or a sticker of Spiderman, or some cartoon) to put on the chart and praise him highly. I suggest you have your doctor check your son out just to be sure his bladder is fine, or that he's not experiencing bowel pain of any kind. As far as your son having a bowel movement get some cheap sparkles from a store and keep it in the bathroom. Tell your son if he poos in the toilet or takes a pee, that he can sprinkle some sparkles in the bowl and flush the toilet. Often children are facinated with these sparkles and will do what you ask just to be able to watch these sparkles disappear down the toilet. There are also Jr. panties you can buy with the kid's favorite cartoon character on them. Try these for a bit. There is Spiderman and Ice Age Characters. Don't fret or get too upset because your son's peers eventually will shame him into going to the bathroom. As far as the puppy, I have one right now and have had many dogs in my life. Like babies they need guidance. Rule of thumb: If you feed a pup or they drink water, count on 15 minutes after that they will need to go outside to do their business and take them outside. When they go pet them and praise them. Dogs are smart and catch on fast. If the pup makes a mistake in the house DON'T HIT THE DOG, but shake your finger at the pup and say "shame." Buy a kennel from a dog groomers (not that expensive) and put a little blanket inside. If your pup makes that mistake shame it with your finger and then put the pup into the kennel for 10 minutes NO LONGER! By hitting a pup (or any age of dog) is not necessary and it will only make a pup confused and make more accidents. Leave some newspaper in an area of your home (out of sight of family) and also train your pup on this. When the pup pees or poos next, put it on the newspaper and keep taking the pup back to the paper, stroke the pup and keep saying "good dog" even if they do nothing. The reason I train my dogs to go on the paper is perhaps my husband and I are out later than expected and the dog shouldn't have to sit home with a full bladder or having to go poo. It wasn't long ago that children were considered "problem children" for bed-wetting, but, doctors have now found that children don't wet there bed constantly because they are too lazy to go to the bathroom, but because their bladders are small and have not grown enough to fit their age level (but will.) Get your husband and boyfriend to help out when they get home so you can have a rest. Good luck Marcy
Do sedimentary rocks absorb water?
Porosity or void fraction is a measure of the void (i.e., "empty") spaces in a material, and is a fraction of the volume of voids over the total volume, between 0--1, or as a percentagebetween 0--100%. The term is used in multiple fields including pharmaceutics, ceramics, metallurgy, materials, manufacturing, earth sciences and construction.Void fraction in two-phase flowIn gas-liquid two-phase flow, the void fraction is defined as the fraction of the flow-channel volume that is occupied by the gas phase or, alternatively, as the fraction of the cross-sectional area of the channel that is occupied by the gas phase.[1]Void fraction usually varies from location to location in the flow channel (depending on the two-phase flow pattern). It fluctuates with time and its value is usually time averaged. In separated (i.e., non-homogeneous) flow, it is related to volumetric flow rates of the gas and the liquid phase, and to the ratio of the velocity of the two phases (called slip ratio).Porosity in earth sciences and constructionUsed in geology, hydrogeology, soil science, and building science, the porosity of a porous medium (such as rock or sediment) describes the fraction of void space in the material, where the void may contain, for example, air or water. It is defined by the ratio:where VV is the volume of void-space (such as fluids) and VT is the total or bulk volume of material, including the solid and void components. Both the mathematical symbols ϕ and n are used to denote porosity.Porosity is a fraction between 0 and 1, typically ranging from less than 0.01 for solid granite to more than 0.5 for peat and clay. It may also be represented in percent terms by multiplying the fraction by 100.The porosity of a rock, or sedimentary layer, is an important consideration when attempting to evaluate the potential volume of water or hydrocarbons it may contain. Sedimentary porosity is a complicated function of many factors, including but not limited to: rate of burial, depth of burial, the nature of the connate fluids, the nature of overlying sediments (which may impede fluid expulsion). One commonly used relationship between porosity and depth is given by the Athy (1930) equation:[2]where ϕ0 is the surface porosity, k is the compaction coefficient (m−1) and z is depth (m).A value for porosity can alternatively be calculated from the bulk density ρbulk and particle density ρparticle:Normal particle density is assumed to be approximately 2.65 g/cm3, although a better estimation can be obtained by examining the lithology of the particles.]Porosity and hydraulic conductivityPorosity can be proportional to hydraulic conductivity; for two similar sandy aquifers, the one with a higher porosity will typically have a higher hydraulic conductivity (more open area for the flow of water), but there are many complications to this relationship. The principal complication is that there is not a direct proportionality between porosity and hydraulic conductivity but rather an inferred proportionality. There is a clear proportionality between pore throat radii and hydraulic conductivity. Also, there tends to be a proportionality between pore throat radii and pore volume. If the proportionality between pore throat radii and porosity exists then a proportionality between porosity and hydraulic conductivity may exist. However, as grain size and/or sorting decreases the proportionality between pore throat radii and porosity begins to fail and therefore so does the proportionality between porosity and hydraulic conductivity. For example: clays typically have very low hydraulic conductivity (due to their small pore throat radii) but also have very high porosities (due to the structured nature of clay minerals), which means clays can hold a large volume of water per volume of bulk material, but they do not release water rapidly and therefore have low hydraulic conductivity.Sorting and porosityWell sorted (grains of approximately all one size) materials have higher porosity than similarly sized poorly sorted materials (where smaller particles fill the gaps between larger particles). The graphic illustrates how some smaller grains can effectively fill the pores (where all water flow takes place), drastically reducing porosity and hydraulic conductivity, while only being a small fraction of the total volume of the material. For tables of common porosity values for earth materials, see the "further reading" section in the Hydrogeology article. Porosity of rocksConsolidated rocks (e.g. sandstone, shale, granite or limestone) potentially have more complex "dual" porosities, as compared with alluvial sediment. This can be split into connected and unconnected porosity. Connected porosity is more easily measured through the volume of gas or liquid that can flow into the rock, whereas fluids cannot access unconnected pores.[edit]Porosity of soilPorosity of surface soil typically decreases as particle size increases. This is due to soil aggregate formation in finer textured surface soils when subject to soil biological processes. Aggregation involves particulate adhesion and higher resistance to compaction. Typical bulk density of sandy soil is between 1.5 and 1.7 g/cm³. This calculates to a porosity between 0.43 and 0.36. Typical bulk density of clay soil is between 1.1 and 1.3 g/cm³. This calculates to a porosity between 0.58 and 0.51. This seems counterintuitive because clay soils are termed heavy, implying lower porosity. Heavy apparently refers to a gravitational moisture content effect in combination with terminology that harkens back to the relative force required to pull a tillage implement through the clayey soil at field moisture content as compared to sand.Porosity of subsurface soil is lower than in surface soil due to compaction by gravity. Porosity of 0.20 is considered normal for unsorted gravel size material at depths below thebiomantle. Porosity in finer material below the aggregating influence of pedogenesis can be expected to approximate this value.Soil porosity is complex. Traditional models regard porosity as continuous. This fails to account for anomalous features and produces only approximate results. Furthermore it cannot help model the influence of environmental factors which affect pore geometry. A number of more complex models have been proposed, including fractals, bubble theory, cracking theory,Booleangrain process, packed sphere, and numerous other models. See also Characterisation of pore space in soil.]Types of geologic porositiesPrimary porosity The main or original porosity system in a rock or unconfined alluvial deposit. Secondary porosity A subsequent or separate porosity system in a rock, often enhancing overall porosity of a rock. This can be a result of chemical leeching of minerals or the generation of a fracture system. This can replace the primary porosity or coexist with it (see dual porosity below). Fracture porosity This is porosity associated with a fracture system or faulting. This can create secondary porosity in rocks that otherwise would not be reservoirs for hydrocarbons due to their primary porosity being destroyed (for example due to depth of burial) or of a rock type not normally considered a reservoir (for example igneous intrusions or metasediments). Vuggy porosity This is secondary porosity generated by dissolution of large features (such as macrofossils) in carbonate rocks leaving large holes, vugs, or even caves. Effective porosity (also called open porosity) Refers to the fraction of the total volume in which fluid flow is effectively taking place and includes Caternary and dead-end (as these pores cannot be flushed, but they can cause fluid movement by release of pressure like gas expansion[3]) pores and excludes closed pores (or non-connected cavities). This is very important for groundwater and petroleum flow, as well as for solute transport. Ineffective porosity (also called closed porosity) Refers to the fraction of the total volume in fluids or gases are present but in which fluid flow can not effectively take place and includes the closed pores. Understanding the morphology of the porosity is thus very important for groundwater and petroleum flow. Dual porosity Refers to the conceptual idea that there are two overlapping reservoirs which interact. In fractured rock aquifers, the rock mass and fractures are often simulated as being two overlapping but distinct bodies. Delayed yield, and leaky aquifer flow solutions are both mathematically similar solutions to that obtained for dual porosity; in all three cases water comes from two mathematically different reservoirs (whether or not they are physically different). Macro porosity Refers to pores greater than 50 nm in diameter. Flow through macropores is described by bulk diffusion. Meso porosity Refers to pores greater than 2 nm and less than 50 nm in diameter. Flow through mesopores is described by Knudsen diffusion.Micro porosity Refers to pores smaller than 2 nm in diameter. Movement in micropores is by activated diffusion. Measuring porositySeveral methods can be employed to measure porosity:Direct methods (determining the bulk volume of the porous sample, and then determining the volume of the skeletal material with no pores (pore volume = total volume − material volume).Optical methods (e.g., determining the area of the material versus the area of the pores visible under the microscope). The "areal" and "volumetric" porosities are equal for porous media with random structure.[4]Computed tomography method (using industrial CT scanning to create a 3D rendering of external and internal geometry, including voids. Then implementing a defect analysis utilizing computer software)Imbibition methods,[4]i.e., immersion of the porous sample, under vacuum, in a fluid that preferentially wets the pores. Water saturation method (pore volume = total volume of water − volume of water left after soaking).Water evaporation method (pore volume = (weight of saturated sample − weight of dried sample)/density of water)Mercury intrusion porosimetry (several non-mercury intrusion techniques have been developed due to toxicological concerns, and the fact that mercury tends to form amalgams with several metals and alloys).Gas expansion method.[4]A sample of known bulk volume is enclosed in a container of known volume. It is connected to another container with a known volume which is evacuated (i.e., near vacuum pressure). When a valve connecting the two containers is opened, gas passes from the first container to the second until a uniform pressure distribution is attained. Using ideal gas law, the volume of the pores is calculated as, whereVV is the effective volume of the pores, VT is the bulk volume of the sample, Va is the volume of the container containing the sample, Vb is the volume of the evacuated container, P1 is the initial pressure in the initial pressure in volume Va and VV, and P2 is final pressure present in the entire system. The porosity follows straightforwardly by its proper definition . Note that this method assumes that gas communicates between the pores and the surrounding volume. In practice, this means that the pores must not be closed cavities. Thermoporosimetry and cryoporometry. A small crystal of a liquid melts at a lower temperature than the bulk liquid, as given by the Gibbs-Thomson equation. Thus if a liquid is imbibed into a porous material, and frozen, the melting temperature will provide information on the pore-size distribution. The detection of the melting can be done by sensing the transient heat flows during phase-changes using differential scanning calorimetry - (DSC thermoporometry),[5]measuring the quantity of mobile liquid using nuclear magnetic resonance - (NMR cryoporometry)[6]or measuring the amplitude of neutron scattering from the imbibed crystalline or liquid phases - (ND cryoporometry).[7]hi im rachelle can you pls add me at: rachelletugagao@yahoo.comthank's and god bless
When was The Get Wets created?
The Get Wets was created in 2006.
When was WETS-FM created?
WETS-FM was created on 1974-02-24.
When was Roger J-B Wets born?
Roger J-B Wets was born in 1937.
Why he will not see you on weekends?
a wets number
What form of matter that flows and wets?
liquid.
A form of matter that flows and wets?
Is it mercury?
Should all kids be required to wear diapers?
If the kid wets itself daily and soils itself I don't think that child is ready for the responsibility of the potty and should go back to diapers
Water wets a glass rod therefore?
13
Who wets their pants more boys or girls?
boys
What did the wets argue for during the prohibition?
legalization of bootlegging
What should you do with a child who wets bed on purpose?
You should diaper them
When a child wets the bed at night it is called?
nocturnal enuresis
