Wednesday, October 28, 2015

The Lichen Study

Lichens are a symbiotic relationship between algae and fungi that cover ten times as much of the surface of earth as tropical rain forests. The fungi are not able to survive without their algal partner and the algae may survive off the photosynthetic properties. Lichen species differ by the fungi present and allows for classification. The lichen body is composed of fungal filaments that encompass green algae cells. Even when there is a low concentration, lichens are able to absorb minerals and water. This synergistic system can withstand intense cold, heat, light and barren rock.

Lichens are significant in determining air quality of an area because of growth sensitive to pollutants. Namely, air pollutants such as sulfur dioxide and nitrogen dioxide. Sulfur dioxide is considered an industrial pollutant and is commonly the by-product of high sulfur fuels; nitrogen dioxide is a common oxide produced by high temperatures in combustion reactions including the burning of coal of fumes from automobiles. Nitrogen dioxide cause alkalinity in lichen substrates while sulfur dioxide disrupts important physiological processes in lichens and can cause acidity. “Lichen deserts,” areas of little to no lichen growth, occur in areas where there are high sulfur dioxide concentrations. This is because photosynthesis and respiration is sensitive to changes in pH and therefore sulfur dioxide rich areas show a decrease in lichen species. On the other hand, a tolerant species has the potential to grow in areas of high pollutant concentrations.

Beatrix Potter, a well-known children’s author, had a passion for botany. She was one of the first to anticipate lichens as symbiotic life forms with records of algal and fungal properties. Potter took the initiative to maintain some algal cells and fungal spores in the heart of her own kitchen. Illustrations demonstrated Potter’s observations suggesting that every twenty minutes fungal and algal growth was monitored. She was forty years ahead of her time with many of the fungal differences not recognized until the 1940s.



Candelaria concolor, a yellow foliose species, contains small lobes and is tight attached to the substrate on which it grows. This species favors nutrient rich bark and is sensitive to sulfur dioxide. Physica species, typically blue or green in color, are abundant if excess nitrogen is in the air. If one of these species is present in an area that is not normally this nutrient rich, the site is considered to be anthropogenically enhanced.

I was put into group B and we covered West Green and the Union Street area. I chose a tree just outside the Life and Sciences Research Building just off Union Street. The tree was very close to the parking lot at only a twelve-step distance. To measure the lichen growth, a four-quadrant contraption was created out of a piece of 11x17 inch paper; each quadrant measured 4x4 inches. The four directions were measured on the tree: north, east, south, and west. This data is going to be used to determine sulfur dioxide and nitrogen dioxide levels in the air on different areas of the campus. This data will include samples from trees on South Green, College Green, and West Green/ Union Street.

The coordinates of my tree on West Green: 39°19’38, 0’N 82°06’15.3’W. I identified the species as Acer rufinerve, a snakebark maple that is native to Japanese mountain forests; the tree exhibited the paired branching. To begin, the measuring device was placed about 1 meter off the ground (close to 3 feet) and held at almost eye level. The northern side of the tree contained the most lichen with a measured 3 in all four quadrants. This was the side where the colonies were visible from across the parking lot with the naked eye. The eastern side of the tree demonstrated the lowest measurement of lichen. Quadrants one, three, and four had a score of 0 while quadrant two had a score of 1. The southern direction of the tree also contained many lichen with scores matching the northern direction. All four quadrants measured a 3. It was difficult to see just how many lichen were on this side because the colonies were so small, however, abundant. These would not have been visible across the parking lot unlike the lichen facing the northern direction. The western direction of the tree was fairly moderate with quadrant one measuring a 3 and quadrant 3 measuring a 1. Quadrant two and quadrant 4 measured a 0.

The standard deviation of the data was then calculated.
            Values:
1.     N: 3, 3, 3, 3
2.     E: 0, 1, 0, 0
3.     S: 3, 3, 3, 3
4.     W: 3, 0,1, 0

Average:
(3+3+3+3) + (0+1+0+0) + (3+3+3+3) + (3+0+1+0) = (12 + 1 + 12 + 4) = 29
29/ 16 values = 1.8125 or 1.81 average

Standard Deviation:
N: 3 – 1.81 = (1.19)2 = 1.41
S: 3 – 1.81 = (1.19)2 = 1.41
     3 – 1.81 = (1.19)2 = 1.41
    3 – 1.81 = (1.19)2 = 1.41
     3 – 1.81 = (1.19)2 = 1.41
    3 – 1.81 = (1.19)2 = 1.41
     3 – 1.81 = (1.19)2 = 1.41
    3 – 1.81 = (1.19)2 = 1.41
E:  0 - 1.81 =  (-1.81)2 = 3.28
W: 3 – 1.81 = (1.19)2 = 1.41
     1 - 1.81 =  (-.81) 2 = .66
    0 - 1.81 =  (-1.81)2 = 3.28
     0 - 1.81 =  (-1.81)2 = 3.28
    1 - 1.81 =  (-.81) 2 = .66
     0 - 1.81 =  (-1.81)2 = 3.28
    0 - 1.81 =  (-1.81)2 = 3.28

Average:
√(1.41 + 1.41 + 1.41 + 1.41) + (3.28 +.66 + 3.28 +3.28) + (1.41 +1.41 +1.41 +1.41) + (1.41 + 3.28 + .66 + 3.28)/ 16-1
=(5.64) + (10.5) + (5.64) + (8.63)/ 15
=30.41/15
=2.023
=1.42


The standard deviation of the data was calculated to be 1.42.



Tree location
Tree location


Paired branching
Paired branching


Northern direction
Northern direction

Eastern direction

Southern direction

Western direction

Sources:

Sunday, October 25, 2015

Stream Erosion

Erosion is the detachment of material from the bed or sides of the stream channel. The erosion of stream banks is considered a natural process caused by the natural flow of water. Disproportionate sediment supply, stream channel instability, land loss, and habitat loss are all adverse effects that depend on the acceleration of this natural process. One possible cause of this acceleration is storms, because they produce storm run-off. Steam bank erosion is not always a problem or in need of fixing. It will become a problem when development (man-made) limits the natural meandering characteristic typical of streams. Stabilizing these areas that do need fixing help protect watercourses from continued sedimentation, damage to adjacent land, control unwanted meander, and improve habitat for fish and wildlife.

 
There are three types of sediment transportation correlating to streams. The first type of sediment transportation is solution load. Solution load is dissolved rock carried in the flowing water. The solution will also contain dissolved salts, calcium, magnesium, and bicarbonate, minerals that have been dissolved from the bedrock. This type of load tends to be higher in areas where bedrock is prone to chemical weathering and where flow is derived from groundwater pathways.

The second type of sediment transportation is suspended load. Suspended load contains finer sediment, mainly clay and silt and fine sand and tiny rocks, suspended by turbulence in the flow by a process called abrasion. A suspended load moves at the same velocity as the flow of the stream. Stream capacity is the maximum load of sediment that a stream can carry and the stream capacity increases with increasing flow velocity. Naturally, streams that contain a greater slop have a greater flow and velocity. Flooding and storms will increase the velocity of the water due to the drastic addition of water to the stream. Stream competence is the largest size material the stream can move. Slow moving streams are highly depositional and are considered a low stream capacity; high velocity streams that can move larger rocks are considered to have a high stream competence. Much of a river’s load is carried in suspension.

The third type of sediment transportation is bed load. Bed load contains courser sediment, mainly sand and gravel, which is too heavy to be carried in suspension and will slide or roll along the stream bed. The amount of bed load will depend on the force exerted by the flow of water, the resisting force of the material in the bed, the climate, the type of bedrock, and the season of the year.  There are two ways of transporting bed loads: traction and saltation. Traction is the scooting and rolling of particles along the bed; saltation is a bouncing movement.


When velocity and discharge decrease, the stream’s ability to move sediment will decrease as well. There are two ways that sediment may deposit on a stream bed: aggradation and bars. Aggradation may raise the elevation of the bed with the accumulation of sediment. Bars are formed when deposits of sand or gravel accumulate and the bars will separate the channel into smaller channels.

Sources: