## The Guide of modifying R Online

If you are curious about Modify and create a R, here are the simple ways you need to follow:

- Hit the "Get Form" Button on this page.
- Wait in a petient way for the upload of your R.
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- Click "Download" to conserve the documents.

## A Revolutionary Tool to Edit and Create R

## How to Easily Edit R Online

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## How to Edit and Download R on Windows

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Mac users can export their resulting files in various ways. With CocoDoc, not only can it be downloaded and added to cloud storage, but it can also be shared through email.. They are provided with the opportunity of editting file through various methods without downloading any tool within their device.

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Google Workplace is a powerful platform that has connected officials of a single workplace in a unique manner. While allowing users to share file across the platform, they are interconnected in covering all major tasks that can be carried out within a physical workplace.

follow the steps to eidt R on G Suite

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## PDF Editor FAQ

## Why do we still study Newton's theories even if Einstein has proven them wrong? Why don't we study Einstein’s theories instead?

OK.Let’s have an example of this.I would like to calculate what speed a ball is travelling at when it hits the ground after I drop it from a height h. How long does it take to hit the ground?I will solve it both ways: once using Newtonian physics, and once using Einstein’s General Relativity. I will use minimal assumptions — just purely using the equations of motion.Let’s see which method is better, right?This answer has a fair amount of mathematics (that’s sort of the point I’m trying to make), so stick with it. You don’t need to understand exactly what I’m doing — just the general gist.The Classical SolutionThe really simple solution to this would be to say that we know that [math]g \approx 9.8[/math]m/s[math]^2[/math], and then use “suvat” to solve it — but that is only an approximation when the gravitational field is constant, which it isn’t. Let’s do the full treatment with a varying gravitational field. It adds a few lines, but you’ll see why we do it later.Newton’s theory (along with Gauss’ theorem) says that we can say that the gravitational attraction due to the Earth (mass [math]M[/math]) on an object of mass [math]m[/math], which is a distance [math]r[/math][math][/math] away from the centre of the Earth, is given by:[math]\displaystyle \mathbf{F} = - \frac{GMm}{r^2} \hat{r} \tag*{}[/math]Since the object in freefall is of constant mass, we can write:[math]\displaystyle \mathbf{F} = m \mathbf{a} = m \frac{\mathrm d \mathbf{v}}{\mathrm d t} \tag*{}[/math]We now make the simplifying assertion that since our ball starts out at rest ([math]\mathbf{v}(0) = 0[/math]), and the only force present is radial in direction, that [math]\mathbf{v}[/math] is only ever radial in direction — i.e. we ignore everything apart from the radial coordinate.This means:[math]\displaystyle \frac{\mathrm d v_r}{\mathrm d t} = - \frac{GM}{r^2} \tag*{}[/math]We now use the following fact:[math]\displaystyle \frac{\mathrm d v_r}{\mathrm d t} = \frac{\mathrm d v_r}{\mathrm d [/math][math]r[/math][math]} \frac{\mathrm d r}{\mathrm d t} \tag*{}[/math]But [math]\frac{\mathrm d r}{\mathrm d t}[/math]is just the radial velocity:[math]\displaystyle v dv = -GM \frac{dr}{r^2} \tag*{}[/math]Integrate, starting from [math]r[/math][math] = R_p + h[/math] at [math]v=0[/math] to [math]r[/math][math] = R_p + x[/math] at [math]v = v(t)[/math].Here “[math]x[/math]" is the height above the ground, and [math]R_p[/math] is the radius of the planet.Hence:[math]\displaystyle v(x) = \sqrt{ 2 GM \left(\frac{1}{R_p + x} - \frac{1}{R_p + h} \right)} \tag*{}[/math]We can now answer the “speed when it hits the ground” question.Setting [math]x = 0[/math], gives:[math]\displaystyle v(0) = \sqrt{ 2GM \left(\frac{1}{R_p } - \frac{1}{R_p + h} \right)} \tag*{}[/math]For a height of 100m, this is:[math]\displaystyle v(0) \approx 44.3 \text{m/s} \tag*{}[/math]The time taken to fall is actually somewhat more difficult — it’s not a particularly nice closed-form expression, but it is the answer to the following integral:[math]\displaystyle t_{fall} = \int_0^h \frac{dx}{\sqrt{ 2GM \left( \frac{1}{R_p + x} - \frac{1}{R_p + h} \right) }} \tag*{}[/math]For [math]h = 100[/math], this comes out as…[math]\displaystyle t_{fall} = 4.5 \text{seconds} \tag*{}[/math]There. That wasn’t too bad, was it?Of course — it’s Newtonian physics, so we know that it must be totally wrong, right?General Relativity SolutionHere’s the General Relativistic approach to the same question — the same height, and the same planet.The equations of motion in GR are the geodesic equations, which take the form[math]\displaystyle \ddot{x}^\mu = \Gamma^\mu_{\nu \lambda} \dot{x}^\nu \dot{x}^\lambda \tag*{}[/math]Where[math]\dot{x}^\mu = \frac{\mathrm d x^\mu}{d p}[/math] where [math]p[/math] is some affine parameter.[math]\Gamma^\alpha_{\beta \gamma}[/math] are the Christoffel symbols derived from the metric.We will model the Earth as being spherically symmetric, which means (by Birkhoff's theorem), it is described by the Schwarzschild metric:[math]\displaystyle -c^2 \mathrm d\tau^2 = g_{\mu \nu} \mathrm d x^\mu \mathrm d x^\nu \tag*{}[/math][math]\displaystyle -c^2 \mathrm d \tau^2 = -c^2 \left( 1 - \frac{R_s}{r}\right) \mathrm d t^2 + \left( 1 - \frac{R_s}{r}\right)^{-1} \mathrm dr^2 + r^2 \mathrm d \Omega^2 \tag*{}[/math]We make our same approximation as before, that there will only be radial motion, so all [math]\theta[/math] and [math]\phi[/math] components drop out.We are therefore left with a need to calculate the following components:[math]\Gamma^r_{r r}[/math][math]\Gamma^r_{r t} = \Gamma^r_{t r}[/math][math]\Gamma^r_{t t}[/math][math]\Gamma^t_{r r}[/math][math]\Gamma^t_{t r} = \Gamma^t_{r t}[/math][math]\Gamma^t_{t t}[/math]Where:[math]\displaystyle \Gamma^a_{b c} = \frac{1}{2} g^{a \sigma} \left( \partial_c g_{\sigma b} + \partial_b g_{\sigma c} - \partial_\sigma g_{bc} \right) \tag*{}[/math]Normally, this would be a whole exercise in itself, but I’m feeling kind today, so I’ll just look them up:[math]\Gamma^r_{r r} = -\frac{GM}{c^2r^2} \left( 1- \frac{R_s}{r}\right)^{-1}[/math][math]\Gamma^r_{r t} = \Gamma^r_{t r} = 0[/math][math]\Gamma^r_{t t} = \frac{GM}{c^2 r^2} \left( 1- \frac{R_s}{r}\right)[/math][math]\Gamma^t_{r r} = 0[/math][math]\Gamma^t_{t r} = \Gamma^t_{r t} = \frac{GM}{c^2 r^2} \left( 1- \frac{R_s}{r}\right)^{-1}[/math][math]\Gamma^t_{t t} = 0[/math]We now perform a transform from our affine parameter [math]p[/math], to the coordinate time [math]t[/math] to give our geodesic equations in the form:[math]\displaystyle \ddot{x}^\mu = -\Gamma^\mu_{\alpha \beta} \dot{x}^\alpha \dot{x}^\beta + \Gamma^t_{\alpha \beta} \dot{x}^\alpha \dot{x}^\beta \dot{x}^\mu \tag*{}[/math]If [math]\mu = t, \theta, \phi[/math], this equation is equal to zero.Hence, we are left with:[math]\displaystyle \ddot{r} = -\Gamma^r_{\alpha \beta} \dot{x}^\alpha \dot{x}^\beta + \Gamma^t_{\alpha \beta} \dot{x}^\alpha \dot{x}^\beta \dot{r} \tag*{}[/math][math]\displaystyle \ddot{r} = -\Gamma^r_{r [/math][math]r[/math][math]} \dot{r}^2 - \Gamma^r_{t t} c^2 \dot{t}^2 + 2 \Gamma^t_{r t} \dot{r} \dot{t} \dot{r} \tag*{}[/math]Plugging in all of the values of [math]\Gamma[/math], and noting that [math]\dot{t} = 1[/math], gives:[math]\displaystyle \ddot{r} = \frac{GM}{c^2 r^2} \left( 1- \frac{R_s}{r} \right)^{-1} \dot{r}^2 - \frac{GM}{r^2} \left( 1- \frac{R_s}{r} \right) + \frac{2GM}{c^2 r^2} \left( 1- \frac{R_s}{r} \right)^{-1} \dot{r}^2 \tag*{}[/math]Which simplifies to:[math]\displaystyle \ddot{r} = \frac{3GM}{c^2 r^2} \left( 1- \frac{R_s}{r} \right)^{-1} \dot{r}^2 - \frac{GM}{r^2} \left( 1- \frac{R_s}{r} \right) \tag*{}[/math]We need to integrate this.Unfortunately, this is not a very nice thing to integrate — you can perfectly well plug it into a computer, and it will do the calculations for you.But we notice that we can plug in some numbers, and for example:[math]\displaystyle \frac{3 GM}{c^2 r^2}\left( 1- \frac{R_s}{r} \right)^{-1} \approx 3 \times 10^{-16} \tag*{}[/math]This is true for all values of [math]r[/math][math][/math] above the planet’s surface.In other words — unless the velocity of our ball is around 20% the speed of light, this term is tiny — absolutely tiny.If the ball is moving at “normal” speeds, then it is of order [math]10^{-13}[/math]In comparison, the second term is approximately [math]10^{16}[/math] times larger — this term is definitely going to be the one that matters.So, we make the approximation that:[math]\displaystyle \ddot{r} \approx - \frac{GM}{r^2} \left( 1- \frac{R_s}{r} \right) + \approx 10^{-13} \tag*{}[/math]But then, we ask — what is [math]R_s[/math]?[math]R_s[/math] is small for a planet the size of Earth — around 9mm.Therefore, [math]R_s/r[/math] is around [math]10^{-9}[/math].Do you think we can ignore that as well? I think we probably can….[math]\displaystyle \ddot{r} \approx - \frac{GM}{r^2} + \approx 10^{-9} \tag*{}[/math]Ah! Now we can solve this!But….But….But….That equation is the almost exact same one that we solved in the classical section of this answer!Classical equation:[math]\displaystyle \ddot{r} = \frac{\mathrm d v_r}{\mathrm d t} = - \frac{GM}{r^2} \tag*{}[/math]GR equation:[math]\displaystyle \ddot{r} \approx - \frac{GM}{r^2} + \approx 10^{-9} \tag*{}[/math]So we spent all that time and effort messing around with GR stuff and metrics….And what does it get us?For a planet the size of Earth, a correction on the order of [math]10^{-9}[/math].Honestly, if you exhaled on the ball on the way down it would have a bigger effect than [math]10^{-9}[/math].We spent sodding ages on that mathematics, and it got us a correction smaller than farting on the goddamn ball.I’m honestly not joking. Accidental nearby flatulence is a more serious correction than General Relativity.So why do we still learn Newtonian mechanics?Because it is so much quicker!Even the method I used in this answer was unnecessarily long and laborious.You can solve the “how fast is it going” question in a single line, using conservation of energy.In general relativity, however?The maths is much, much, much harder — and we weren’t even dealing with any of the conceptually difficult stuff, this was just raw number crunching.And how much more accurate was it?It was no more accurate.To all intents and purposes, both results gave the exact same answer.Relativity is necessary in some regimes — but in the “everyday” regime….using General Relativity is like googling how to spell your own name.Sure, you’ll get the right answer, but there are quicker ways to do it….So that is why we still learn Newtonian mechanics — because 99.99% of the time there is no realistic difference between the two answers.Using General Relativity is a pain.You want to avoid it and use approximations as often as possible.And Newtonian mechanics is a bloody good approximation.

## What are the real reason(s) Toys R Us went bankrupt?

There are a lot of reasons why Toys“R”Us went bankrupt, but the simple answer is that the owners (KKR, Bain and Vornado Realty Trust) made a gamble and lost. That’s combined with a secret that few outside of the industry knew - Babies“R”Us tanked everything.Toys“R”Us was purchased in a leveraged buyout by these three companies in 2005. The goal was to take TRU private, fix the issues, make it profitable, go public and make a ton money. This saddled Toys“R”Us with about $5 billion in debt, restricting their ability to actually do thingsIn 2005, the U.S. toy business was weak (hammered by Walmart), but the Babies“R”Us business was keeping the company afloat.In 2010, the company filed for an IPO, but all of the above changed. The toy business had seen significant growth in sales and market share vs. competitors. But, the baby business never saw Buy Buy Baby or Amazon coming after it and became an anchor around the company.Also, while the business was growing, a substantial piece of the numbers were based on combining Toys and Babies stores together. You saw a double-digit sales increase, but that level of increase couldn’t be annualized. And, it essentially created a 5-year plan that could have sustained the company through an IPO in 2010 - 2012.Also, this was in the middle of the financial crisis. So, while the IPO was filed, some of the owners wanted to wait until they could get more money. That pushed back the execution of the IPO, while, unfortunately, Toys“R”Us sales started to decline. That made them less attractive to investors, and ultimately led to them rescinding the intent to file the IPO in 2013 (I don’t know the technical terms).Delaying the IPO for better market conditions is the bet the owners lost on. And, if they had filed, Toys“R”Us could have paid its debt.So, the reason the liquidation is happening now is that last September, they retained a bankruptcy lawyer (I don't know the specifics, but I believe they were concerned about the possibility of missing a payment). That set off a chain reaction of manufacturers not shipping products, which destroyed their holiday sales. That led to nobody being willing to lend them money, which led to liquidation. And here we are.

## What is the most satisfying solution of [math]y=\frac{\ln(\chi) + (s a - 1) \ln(m)}{r^2}[/math]?

Nice![math]r\cdot r\cdot y=\ln\chi+\ln m^{sa-1}[/math][math]r\cdot r\cdot y=\ln\chi m^{sa-1}[/math][math]e^{r\cdot r\cdot y}=\chi m^{as}\cdot m^{-1}[/math][math]me^{rry}=\chi m^{as}[/math]

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