Soil Horizons Explained

Thursday, April 30, 2020




Soil  Profile and Horizons Explained

Soil is all around us Soil is essential. You walk on grass rooted in the soil and eat food grown in soil.
Plants and trees need soil to grow but
What is soil composed of

If you look at a chart of soil you will see that Soil is made up of,

45%  minerals
5%    organic matter like decaying plants and animals
25%  water
24%  air

You can also study soil by looking at the soil profile and the soil horizon
A vertical layer of soil that shows all of the different layers is the soil profile.
Much like your profile on Facebook tells others all about you The profile tells others all about the soil

A soil horizon is each individual layer of the profile. Each layer has different physical properties.

Learn the difference between soil profile and the soil horizons.
The soil horizons are the horizontal layers of the soil. The layers are o a e b c r. 

O horizon also called litter is composed of dead leaves, twigs, sticks, fallen trees The O horizon is thin in some soils, thick in others, and not present at all in others.

A horizon also called topsoil Contains rich organic matter along with some minerals. This layer contains decomposers. The decomposers perform the task of breaking down plants and animals. The remains of these plants and animals create a mixture called humus which is a dark, organic material that forms in soil when plant and animal matter decays.

E horizon also is known as the Eluviated layer as water moves down the soil substances are removed and pulled out in this layer resulting in a concentration of sand and silt particles composed of quartz or other resistant materials This layer may be missing in some soils.

B horizon Subsoil Lighter in color, many times reddish or brownish in color because it has less humus it is a zone of accumulation where materials like clay collects from the movement of water downward

C horizon Parent material this layer contains much of the material that the soil was originally made from. It will contain rock fragments. Weathering breaks down this parent rock into smaller and smaller pieces of rock This layer is most often light in color.

R bedrock  A mass of rock such as granite, basalt, quartzite, limestone, or sandstone that forms the parent material for some soils.












Landforms created by Erosion.

Thursday, April 23, 2020


Erosion is the process by which sediment and other materials are moved from one place to another. There are four main agents of erosion, wind, water, ice, and waves.
A deposition is a geological process in which sediments, soil, and rocks are added to a landform or land mass.
Erosion and deposition have taken place throughout Earth’s history and have created a variety of landforms.
What landforms have been created by erosion?
Canyons and valleys pause
Canyons and valleys are created by the flow of water. As the water moves, it erodes rock and sediment from the streambed.
The steeper the river or stream the greater the erosion force. 

Erosion and deposition can form a flat area called a floodplain

When a stream empties into a body of water such as the ocean, an estuary, a lake, or reservoir. It’s current slows and sediment is deposited. A fan-shaped pattern is formed called a delta that can be created. 

An alluvial fan is created when the stream flows onto land. They are sometimes associated with flash floods. These fans typically form in mountain regions where there is a rapid change in slope from high to a gradual slope. When the land flattens out the flow of water loses energy and deposits sediment in a fan shape.

A meander is a bend in a river. The faster-moving water on the outside cuts into the bank. On the inside of the curve, water moves more slowly and deposits sediment. Sometimes a stream may cut a new channel that bypasses the meander. This cutoff meander may form a lake called an oxbow lake.

Groundwater can also be an agent of erosion
The groundwater dissolves and carries rock away and may create a cave.
If the roof of the cave collapses it may create a sinkhole.
The world's largest sinkhole. A sinkhole in Egypt is considered the largest in the world. It measures a staggering 80 kilometers long and 120 kilometers wide. Yes, that is kilometers not meters.

If you would like to know more about landforms this playlist you may enjoy this playlist.







10 Interesting facts about Mitochondria

Tuesday, April 21, 2020




Mitochondria are essential for the production of proteins, RNA, pumps, and several other essential processes in the cell.  Mitochondria are amazing and cool.
They are found in plants... animals,....fungi,.....protists, and any other eukaryotic cell.

Let's Learn 10 Facts about Mitochondria
1. They can quickly change shape and move around the cell when needed.

2. When the cell needs more energy, the mitochondria can reproduce by growing larger and then dividing. For example, say you want to get in shape. As you exercise more of the mitochondria in your muscles will increase in number and navigate to the edges of the cell, which allows these muscle cells to have more energy.

3. If the cell needs less energy, some mitochondria will die or become inactive. 

4. Mitochondria are very similar to some bacteria. For this reason, some scientists think that they originally were bacteria that were absorbed by more complex cells. This theory is called endosymbiosis.

5. During cellular respiration, with the help of oxygen, the mitochondria produce 25 ATP compared to only 3 ATP produced during glycolysis in the cytoplasm.

6. ATP is continuously broken down into ADP, like a rechargeable battery, and releases a huge amount of energy which is used by the cell in several metabolic processes as well as in building macromolecules such as proteins.

7. ATP is critical for the contraction of muscles.

8. ATP supplies the energy to move the contractile muscle proteins.

9. ATP is essential for certain pumps like the sodium-potassium pumps and calcium pumps. The sodium-potassium pump ensures that our cells have the correct amount of sodium and potassium which is essential to stay alive.

10. The adenosine from ATP is a building block of RNA and is directly added to RNA molecules. During Transcription DNA is copied to mRNA, which carries the information needed to make proteins. 

How to Read and Write a Decimal

Friday, April 17, 2020

How do you read 24.076?
If you follow a couple of simple rules it can be really easy.
Decimals are used to measure small amounts and small objects like the width of a hair. Your hair is only zero and four-hundredths of a millimeter wide. Ants are only zero and 75 hundredths of a centimeter in length.

Let's review a couple of items that will help when reading and writing a decimal.

Decimals are to the right of the decimal point.

Instead of increasing by ten times the number like numbers to the left of the decimal point do
numbers to the right of the decimal point are ten times smaller.
Notice that there are no ones involved with these numbers to the right of the decimal.

You start at tenths then hundredths thousandths, and so on. Notice the "th"  at the end of each decimal place name.

A decimal number has three parts.

A whole number, a decimal number, and a fractional part.

In order to read a decimal start at the far left. 
1. At the decimal point say "and"

2. Then read the number after the decimal point. 

3. The last step is to say the name of the place of the final digit.

Let’s read the decimal number 2.54.

Two and 54 hundredths


Remember the ths at the end.

Let's Read 0.5

 Zero and 5 tenths

How about 0.0363?

 Zero and three hundred and sixty-three ten thousandths
Read
72. 4 
Seventy-two and four-tenths.




Transition Metals

Monday, April 13, 2020



Which group of metals are silver, maybe gold, and sometimes liquid?

The transition metals


The transition metals are the elements found in groups 3-12

According to the International Union of Pure and Applied Chemistry. A transition metal is an element with a partially-filled d subshell or the capacity to produce cations with an incomplete d subshell.

Using this definition, here is a list of 40 transition metals with their number of valence electrons.
21 Scandium 2
22 Titanium 2
23 Vanadium 2
24 Chromium 1
25 Manganese 2
26 Iron 2
27 Cobalt 2
28 Nickel 2
29 Copper 1
30 Zinc 2
39 Yttrium 2
40 Zirconium 2
41 Niobium 1
Molybdenum 1
Technetium 2
Ruthenium 1
Rhodium 1
Palladium 18
Silver 1
48 Cadmium 2
71 lutetium 2
72 Hafnium 2
73 Tantalum 2
74 Tungsten 2
75 Rhenium 2
76 Osmium 2
77 Iridium 2
78 Platinum 1
79 Gold 1
80 Mercury 2
103 Lawrencium 3
104 Rutherfordium 2
105 Dubnium 2
106 Seaborgium 2
107 Bohrium 2
108 Hassium 2
109 Meitnerium 2
110 Darmstadtium 1
111 Roentgenium 2
112 Copernicium 2

Technically, the elements zinc, cadmium, and mercury which are found in Group 12 should not be considered transition metals because they have a full d10 configuration
Copernicium should probably be excluded on the same basis. However, most people include these elements in the transition metal list. There are also scientists and educators who include the full lanthanide and actinide series as transition metals. The transition metals are metallic elements that serve as a bridge, or transition, between the two sides of the table. The group elements with s orbitals and p orbitals.

The lanthanides and the actinides at the bottom of the table are sometimes known as the inner transition metals.
Most transition metals are like most metals and appear shiny and metallic with a grayish or white color. However, gold and copper have their own unique colors. Most have high melting points, but mercury is liquid at room temperature.

Although the transition metals are reactive, they are not as reactive as elements belonging to the alkali metals group.
Most transition metals have 2 electrons in their outer shell,but some have 1 electron and Palladium has 18.
They are good catalysts. They are paramagnetic which means they are attracted to a magnetic field. They are good electrical and thermal conductors.

They form alloys. An alloy is a combination of metals in which combine with one or more other elements. For example, iron combines with carbon creating steel.



Erosion of rocks

Thursday, April 9, 2020

What is the erosion of rocks?


How was this cave carved out of solid rock? 

cave showing erosion

Weathering and erosion worked together to create the cave.

Weathering breaks the rock down then erosion carries this rock away

Erosion happens when rocks and sediment are picked up and moved to another place by the water, wind, ice, and even gravity. Erosion can occur slowly over time like a sand dune or quickly like a flood.

There several methods of erosion.

Remember, weathering breaks down the rock, and erosion moves the rock away

Rainfall can cause erosion and wash sediment away

Valley erosion occurs when rushing streams and rivers move rocks and sediment downstream. 

Oceans are a huge force of erosion.

Wind can cause erosion. 

Here are a couple more agents of erosion.

A dust storm can be a huge force of erosion.

dust storm



Ice and glaciers erode rock. 
Greenland and Antarctica have huge glaciers that move rock from one area to another.

Remember  Weathering breaks down rock and erosion moves this rock away.

Related Links





Physical and Chemical Weathering of Rocks

Wednesday, April 8, 2020



Weathering of rocks is a physical or chemical change that changes the characteristics of rock on earth 
There are two major types of weathering.

Chemical weathering changes which involve rocks being changed into new substances or new minerals chemically.

chemical weathering




Physical weathering involves breaking rocks into smaller fragments caused by environmental factors.

weathering


Three major types of physical weathering
  • Abrasion
  • Frost Wedging
  • Thermal stress
Abrasion is a mechanical scraping and can be caused by the following factors.
  • Wind
  • Water /waves
  • Glaciers
  • Gravity
  • Plants/animals
Frost wedging occurs as water expanding as it freezes causing the rock to break apart.

Thermal stress results when heat and changes in temperature cause rock to expand and contract and this can break the rock apart. 
Chemical changes occur when a chemical reaction creates a new substance.


Oxidation occurs as oxygen o2 combines with iron in rock and creates new compounds.

When iron reacts with oxygen, it forms iron oxide commonly called rust, which weakens the rock.

oxidation


Hydrolysis occurs when hydrogen reacts and creates a new substance.
For example, Hydrolysis causes feldspar to turn into clay.

Carbonation is the process of mixing water with carbon dioxide to make carbonic acid. This acid then breaks down and weakens rocks. Caves may be formed by carbonation dissolving limestone. Rainwater picks up carbon dioxide from the air and as it percolates through the soil slowly dissolves out the limestone.


Helpful Resources on weathering


Weathering Playlist


Weathering Crossword Puzzle

The Mohs Scale of Hardness Explained

Sunday, April 5, 2020



The Mohs scale of mineral hardness is based on the ability of one mineral to scratch another mineral visibly. The Mohs' hardness scale was developed in the 1800s by Frederich Mohs, a German mineralogist. 
Hardness is a measure of a mineral’s ability to resist being scratched. He selected ten minerals of different hardness that ranged from a very soft mineral (talc) to a very hard mineral (diamond). 
When completing hardness tests of the minerals it is necessary to determine which mineral was scratched.

Let’s go through the Moh’s Scale

As you move up the scale hardness increases

1 Talc

2 Gypsum

3 Calcite

4 Fluorite CaF2

5 Apatite

6 Orthoclase feldspar

7 Quartz

8 Topaz

9 Corundum

10 Diamond

You can also use common household items to test for hardness.

  • A fingernail 2-2.5
  • Penny 3.5
  • Nail 5-6
  • Glass 5- 5.5
  • Streak plate 6 6.5
  • Quartz 7
Let's determine the hardness of a mineral. The mineral can scratch talc so it has a hardness greater than 1. However, the mineral can be scratched by calcite which has a hardness 3 so its hardness is 2.

Now I can use this information, along with a mineral field guide in order to identify the mineral.

Additional Mohs Scale Resources


Mohs scale on Youtube

Helpful Article

A very detailed list of Mineral and Hardness

Practice Identifying Minerals

Thursday, April 2, 2020


First, what makes a mineral a mineral?

*A mineral is,
*Naturally Occurring
*Inorganic solid
*Crystalline Structure
*Same chemical composition throughout

This chart goes along with the video identifying minerals.

Use this blank chart during the video in order to record data.


Number
Color
Luster
Streak
Color
Hardness
Reaction with Vinegar
Magnetic


















































Use this chart in order to identify the minerals based on physical properties.


Mineral
Color
Luster
Streak
Color
Hardness
Reaction with Vinegar
Magnetic
Feldspar
White
Red
Green
Glassy
Vitreous
White
6
No
No
Hematite
Red,
Black
Brown
Dull
metallic
red
5.5 6
No
No
Pyrite
Brass
Yellow
metallic
brown
6
No
No
Quartz
No color
White
Glassy
vitreous
none
6.5  7
No
No
Mica
No
color
Yellow

glassy
none
white
2
No
No
Magnetite
Black
metallic
black
6
No
Yes
Calcite
white
Glass
vitreous
white
2.5 3
Yes
No
Talc
White
Green
Gray
Greasy pearly
white
1
No
No



Answer Key

Mineral #1 Talc

Mineral #2  Magnetite

Mineral #3 Mica

Mineral #4 Calcite

Mineral #5 Quartz

Mineral #6 Pyrite

Mineral #7 Feldspar

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