Thankyou so much for your help again geodome, and Mark.
I had a look at your answer and worked on it myself until i got the same answer, my working is very similar too.
rate=k.[A]3
-(d[A] / dt) = k.[A]3
separating variables:
-(d[A] / [A]3) = k.dt ----> -[A]-3.d[A] = k.dt
First working on the left hand side:
integrate -[A]-3d[A] from [A]o to [A]t = [-[A]-3+1 / -3+1][A]t[A]o
= [-[A]-2 / -2][A]t[A]o
= [1/2[A]-2 ][A]t[A]o
= [1/2[A]-2 t ] - [1/2[A]-2 o ]
= 1 / {(2). [A]2 t} - 1 / {(2). [A]2 o}
>Now working on the right hand side:
integrate k.dt from o to t,
this just ends up being " k . (t - o) " which equals " k . t "
>after integrating both sides:
1 / {(2). [A]2 t} - 1 / {(2). [A]2 o} = k . t
>To find the half life:
[A]2 t = (10 mol/L)2 t
[A]2 o = (20 mol/L)2 o
{ 1 / ( (2)(10 mol/L)2 t ) } - { 1 / ( (2)(20 mol/L)2 o ) } = k . t1/2
>which simplifies to:
( 1 / 200 ) - ( 1 / 800 ) = ( 3 / 800) = k . t1/2
>simplifies again:
(3)* { 1 / ( (2)(20 mol/L)2 o ) } = ( 3 / 800) = k . t1/2
>rearranging:
{ 3 / ( (2)(20 mol/L)2 o ) } = k . t1/2
>And now solving for t 1/2 :
k . t1/2 = { 3 / ( (2)(20 mol/L)2 o ) }
t1/2= { 3 / ( (2)(20 mol/L)2 o (k) ) }
Therefore the final expression for half life is:
t1/2 = { 3 / ( (2)[A]2 o (k) ) }
I hope ive made sense with my working, this is pretty full on stuff, for me anyway!
Cheers,
madscientist :albert: