Add Papers Marked0
Paper checked off!

Marked works

Viewed0

Viewed works

Shopping Cart0
Paper added to shopping cart!

Shopping Cart

Register Now

internet library
Atlants.lv library
FAQ

Great deal: today with a discount!

Regular price:
1,99
You save:
0,32 (16%)
Discounted price*:
1,67
Purchase
Add to Wish List
ID number:806510
Author:
Evaluation:
Published: 28.04.2021.
Language: English
Level: Secondary school
Literature: n/a
References: Not used
Extract

Conclusions
At the waters surface is floating junk and bits of peat and some of it later on settled down.
Once the samples have completely settled I put the ruler against the side of the jar to measure the depth of the soil sample. The total depth of soil is 5.6 cm. The clay layer is about 0.1 cm, silt layer about 2 cm and sand layer 3.5 cm.
These measurements I divide like this:
1 mm / 56 mm = 0.018mm
20mm / 56mm = 0.357mm
35mm / 56mm = 0.625mm
Then I multiply these up by 100 to get the average percentage.
The clay layer is 2%
The silt layer is 35%
The sand layer is 63%
The best ratio is when the sand and silt layer is 40% each and clay layer is 20%.
In conclusion from where I took soil, that place will need a lot of watering because the sand is much too high and the clay is really low. The sand can dry up real quick but the clay holds on to water very well.…

Editor's remarks
Work pack:
GREAT DEAL buying in a pack your savings −3,62 €
Work pack Nr. 1385786
Load more similar papers

Send to email

Your name:

Enter an email address where the link will be sent:

Hi!
{Your name} suggests you to check out this Atlants.lv paper on „Soil Types - Experiment”.

Link to paper:
https://eng.atlants.lv/w/806510

Send

Email has been sent

Choose Authorization Method

Email & Password

Email & Password

Wrong e-mail adress or password!
Log In

Forgot your password?

Draugiem.pase
Facebook
Twitter

Not registered yet?

Register and redeem free papers!

To receive free papers from Atlants.com it is necessary to register. It's quick and will only take a few seconds.

If you have already registered, simply to access the free content.

Cancel Register