ipl-logo

Nt1310 Unit 3 Lab Report Sample

474 Words2 Pages

Figure 6 shows the glass container with a soil that is susceptible to liquefaction. The proponents provided a set of containers to observe different data.
Scanning Electron Microscope (SEM) Test
In a certain sample sent in Mindanao State University, Iligan City for SEM (Scanning Electron Microscope) test, results show that the bacteria reacted from the water of the soil which produces chemical reaction and affects the physical attribute of the soil. Image below shows that a limestone like structure really exists in the soil where Bio-Vege Grout was injected.

Figure 7 shows the image without grout being magnified 1000 times its normal appearance. There are voids in the middle and the soil is not compact. There is no presence of the limestone like particle.

Figure 8 shows the image without grout being magnified 500 times its normal appearance. There are voids in the middle and the soil is not compact. There is no presence of the limestone like particle.
Figure 9 shows the images of soil with 50% grout that is magnified 500 times its normal appearance. The soil is compact and there are small particle which is the limestone-like created by the Bio-Vege Grout through chemical …show more content…

The elements needed for calcium carbonate precipitation (CaCO3) are calcium, carbon and oxygen which is present in the table 2 shows the elements present in the soil being tested in the scanning electron microscope (SEM). Carbon has a total mass percentage of 16.1, oxygen has a total mass percentage of 12.16, and Calcium has a total mass percentage of 2.46. Calcium carbonate (CaCO3) is an important chemical compound made up of one atom of calcium (Ca) bonded to one atom of carbon (C) and three atoms of oxygen (O). Its molecular formula is (CaCO3). It only proves that calcium carbonate (CaCO3) precipitation occurred in the soil because of the Bio-Vege

Show More
Related
722 Words | 3 Pages

The rocks do not show signs of heavy weathering. There is some white staining visible, but there is very little red or brown staining. The rocks have abundant vesicles. There is a mix of rocks with varying sizes and numbers of vesicles. Samples collected were representative of this mix.

Read More
1724 Words | 7 Pages

We walked along the beach a little more and talked and looked at the location of a whale skull that used to be buried in the sand. The rock was actually much smoother than . We also took a look at some possible bones and skeletal remains along with concretions. The concretions were rather large comparable to smart car in size. Concretions are solid masses formed around some type of matter that will change the chemistry of the rock slightly, helping it become harder and less susceptible to erosion.

Read More
561 Words | 3 Pages

This cave is located 1000 feet underground and contains many of the largest natural gypsum crystals in the world (2). These pillars of selenite gypsum measure up to 50 feet long and 4 feet in diameter (1). These crystals were able to form in such huge quantities because the area was submerged in water that was rich in minerals as well as having a high stable temperature of 136 degrees Fahrenheit (2). The water had an abundant amount of anhydrite and, because of this environment, it dissolved into gypsum and formed these massive crystals (2). The water has since drained out of the caves and the air in the caves normally stays between 45 and 50 degrees Celsius and the humidity levels range from 90 to 100 percent (3).

Read More
672 Words | 3 Pages

The loamy sand appeared in the A horizon which is considered to be the top soil region. Loamy sand is characterized by containing approximately 25% medium coarse sand particulates, 25% very coarse sand, and less than 50% fine sand and very fine sand (USDA, n.d). The larger the soil particles the less hydrophilic the soil is. Many horticulturalists find that loamy soils are very productive because of their ability to retain water while also draining well (Lerner). This can therefore explain the high levels of vegetative growth in the three locations the soil texture was present in.

Read More
828 Words | 4 Pages

These conditions include soils with antimicrobial matrix, very dry and very cold climates, and oxygen-free environments (Fagan

Read More
1126 Words | 5 Pages

These results were collected because of the In the experiment it was tested how much water was able to pass through three different types of soil. The control in the experiment was no soil for the water to pass through and an average of 39 ml. Passed through. Variable one was gravel and an average of 34 ml.

Read More
509 Words | 3 Pages

Limes tone is usually pure calcium carbonate, but dolomitic limestone has calcium carbonate and magnesium so lows the pH and gives magnesium to the soil. You should not use sulfer that is powdered because it is expensive and it is finer. both limestone and sulfer are not soluble in water so you must place it 6 inches in the soil, must be a quick action. If not possible leave it on top and let it sink in the

Read More
497 Words | 2 Pages

I had lost Limesto while I was grinding. The sediment was carried to a lake through a stream. In the lake we went through deposition. My sediment started sinking until it fell to the floor. Soon more layers fell on top.

Read More
1567 Words | 7 Pages

Lastly the modified environment will have acidic soil instead of sand/dirt in the

Read More
1911 Words | 8 Pages

These results showed that the preparation layer is a mixture of lime (CaO) and sand (SiO2). The presences of S essentially owed to the pollution of sulphure dioxide. The occurrence of Na and Cl are indicative of the existence of halite (NaCl), whose presence is due to materials used in the ground layer or moisture. The presence of aluminum oxide and potassium oxide are from dust. The presence of MgO owed to limestone which had been used in makes lime.

Read More
865 Words | 4 Pages

Carbonation is the reaction of lime with carbon dioxide from the air to form weak cementing agents, notably calcium carbonate (CaCO3). This is undesirable(Bell, 1993). Becoming unstable, calcium-silica, calcium-alimino and calciumalumino-silica hydrates may react with carbon dioxide to revert back to silica, alumina, and calcium carbonate if the pH of the lime-stabilized soil drops sufficiently low. Carbonation reactions are harmful to the long-term strength and durability of the lime-stabilized soil. Using sufficient amount of lime (to provide enough alkalinity), compaction of the soil to high density and prompt placement after mixing lime with soil (to minimize carbon dioxide penetration) can minimize potential carbonation problems.

Read More
531 Words | 3 Pages

Dirt is made up of minerals, particles, and other 10’s of billion organisms that live beneath the ground according to the film “Dirt”. What a great movie it somewhat summarizes our NRES 251 soils class. The movie Dirt is about all aspects of soil such as industrial farming, urban development, mining, and how it endangers the soil. That’s not all the movie also includes scientist and farmers, and ranchers all around the world that admire dirt and believe it’s the most important thing on earth for all living things to exist.

Read More
763 Words | 4 Pages

Both of these materials also were inserted to catch very fine particles that might make their way down the early levels of the fitler. We then have an intermediate layer which consisted of a abrasive pad, and on top of that was a round scrubber surrounded by sand. We hoped that

Read More
861 Words | 4 Pages

This accounts for the rich agricultural deposits in Ohio. As a result, the land is adequate for landfill exploration. Consequently, Ohio soil contains huge amounts of fossils, silt, clay sand, and gravel. The weathering process during the Cenozoic era accounted for the huge mineral deposit in Ohio. The dominant sedimentary deposits include chemical and siliciclastic.

Read More
2041 Words | 9 Pages

Mineralization of carbon and nitrogen in soil are caused by soil organisms that eat organic matter (Meister,

Read More

More about Nt1310 Unit 3 Lab Report Sample

Related Topics

Open Document