Fifth Lab Report (Overall Report) : "Ulam Raja"
SS11403 SAINS TANAH SEKITARAN
SEMESTER 2 2017/2018
Date of Submission: 8th May 2018
MRS. DIANA DEMIYAH BINTI MOHD HAMDAN
TITLE : 'ULAM RAJA' Overall Report
NAME
|
IC NUMBER
|
MATRIC NUMBER
|
MOHD FATHULIZZAT BIN ASFI
|
970528125555
|
BS17110533
|
CHIN JIA HUI
|
970616125600
|
BS17110550
|
RINA BINTI SARIKA
|
981008125096
|
BS17110233
|
MAIZATUL AKMAR BINTI MOHAMAD NIZAM
|
970130235172
|
BS17110366
|
NORFARAH A'AINA BINTI BAHARIN
|
980118126298
|
BS17160676
|
NOOR HIQMAH BINTI MASBOL
|
980607015214
|
BS17110045
|
1.0 INTRODUCTION
There are 4 main factors which affect
the growth of plant, which incude the fertility of soil, the moiture content in
the soil, light intensity as well as the temperature. As you can tell, plants
are similar to human and animal which need nutrient to grow. The total amount
of nutrient that contain in the soil is directly affect the soil fertility. The
more nutrient that the plants can get from the soil indicate high fertility of
the soil. Next, the moiture content also play an important role in growth of
plant as plants absorb water from the soil and they need water to carry out
transpiration as well as photosysthesis. Besides, the moiture content is the
most important factor espcially during the germination phase, deficiency in
water can definitely fail the germination of plant. Where for light intensity, plants
need light energy to carry out photosysthesis. Without light energy, plants
cannot make their own food, reproduce and survive. As plants are autotrophs,
meaning they make their own food source. Lastly, temperature, plants can only
survive in the suitable condition, meaning some plants only can survive in high
temperature where some of them can only survive in cold weather. Therefore a
suitable temperature and condition are needed. Besides of these mentioned
factors, other factors such as soil texture, soil pH, water holding capacity
and permeability also affect the growth rate and the germination of plant .
Cosmos caudatus, also kenikir
in Indonesia or ulam raja which meant "the King's salad"
in Malaysia. The leaves of this plant are commonly use for salad and cooking. Ulam,
is a widely popular Malay herbal salad that is served throughout Malaysia and refers
to a group of traditional Malay vegetables, usually consumed raw. Ulam Raja is
an
annual which can grow
up to 2 m in height. Ulam Raja is a popular herb used in Malay cooking. Their leaves are soft and pungen and tastes
like mild mango, the unique taste makes it a flavorful, and serve as side dish
which usually eaten with chili paste to enhance the flavors. While the stem is
light green in colour with a purplish hue and their flowers are produced on a
single stalk on auxiliary heads.
2.0 OBJECTIVES
1. To identify the most suitable soil to grow Cosmos
caudatus, because different soil hold different pH value, water holding
capacity, nutrient, permeability and salinity of soil. As different plant can growth at different condition.
2. To study the relation of how moisture
content, soil texture and soil fertility can affect the growth of Cosmos
caudatus.
3. To analyse the growth rate of Cosmos
caudatus with the soil minerals and photoavailability.
4. To identify the deficiency symptoms atCosmos
caudatus plants in 4 weeks of germination. The deficiency symptoms shows that
the soil lack some of te nutrient needed.
3.0 METHOD & MATERIAL
1. Ulam Raja
seeds
2. 5 pots ( with hole )
3. 500ml recycle bottle (for watering)
4. 5 different type of soil texture (divide to two
portion which is one portion for soil medium and the other one for lab
analysis)
5. Record GPS coordinate soil sample location was
recorded.
Figure
1 Kokol Hill
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Figure 2 ODEC, UMS
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Figure 3 UMS Peak
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Figure 4 Kg Excellent
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Figure 5 Faculty of Science and Natural Resources (FSSA) Lake
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6. 5 recycle empty transparent bottle
glass jar for soil texture analysis (same size, smooth surface).
7. 5 empty recycle tin can with same
size and poke same number of holes at the bottom of the can.
8. 10 Recycle plastic container for
air-dry soil.
9. Masking tape (for labelling jars)
10. Permanent marker pen
PROCEDURES
1.
2/3
pot was filled up with ground soil .
2.
The
soil was patted to compress the soil so that the level of soil will not shrunk
after watering.
3.
Ulam Rajaseeds were divided equally to
each pots which is 18 seeds in each pots.
4.
2cm
thick of soil was placed on top after the seeds were placed on the soil.
5.
The
pot were labelled by using permanent marker before been placed at the corridor
outside the laboratory.
6.
Then,
the pot was watered with 500ml of water.
7.
Steps
1 to 6 were repeated for Hill soil from UMS Peak, Red soil from Kg E, Wetland
soil from FSSA lake and sandy soil from ODEC.
8.
The
soils were watered two times a week until 26th of March 2018.
9.
26th
of March 2018 to 27th of April 2018 the soils will be watered once a week only.
10. The lab soil tests was
conducted based on the schedule given (Soil Colour Analysis, Soil Texture
Analysis, Soil Moisture, Soil pH, Soil Water Holding Capacity, Sieve Analysis,
Soil Permeability Test, Soil Salinity Test, and Soil Nutrient Analysis).
4.0 RESULT
AND OBSERVATION
Table 1 : Plant Development
WEEK
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DATE
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OBSERVATIONS
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3
|
29 March 2018
|
Figure 1 The seeds were started to germinate in some pots.
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Figure 2 Ulam Raja started to germinate in pot of ground soil. The height was 6 cm.
|
||
Figure 3 Ulam Raja and other plant species were started to germinate in pot of
wet soil. The height of Ulam Raja is 2 cm.
|
||
Figure 4 There were no Ulam Raja germinate in the pot of hill soil but, some
species of plant were started to germinate.
|
||
Figure 5 There were no Ulam Raja or plant germinate in pot of red soil.
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||
Figure 6 There were no Ulam Raja or plant species germinate in pot of sand.
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||
4
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4 April 2018
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Figure 7 Ulam Raja were kept growing until the height was 8.3 cm in ground
soil’s pot
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Figure 8 Ulam Raja and other plant species were kept growing until the height
of Ulam Raja was 4.2 cm in wet soil’s pot.
|
||
Figure 9 The other plants were kept growing in hill soil’s pot.
|
||
Figure 10 Pot of red soil still no germination of any species occur.
|
||
Figure 11 Pot of sand still no germination of any species occur.
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||
6
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17 April 2018
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Figure 12 Ulam Raja kept growing until the height was 16.7 cm in ground soil’s
pot .
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Figure 13 Germination of 3 Ulam Raja and the other plant species in wet soil.
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||
Figure 14 The other plant species kept growing in hill soil.
|
||
Figure 15 Red soil and sand were still have any germination of any species of
plant.
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||
7
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23 April 2018
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Figure 16 Ulam Raja kept growing until the height was 23 cm in pot of ground
soil.
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Figure 17 3 of Ulam Raja kept growing until they height were 9 cm, 6.5 cm and
6.3 cm in pot of wet soil.
|
||
Figure 18 The other plants were still growing while no germination of Ulam Raja
occur.
|
||
Figure 20 The different germination of Ulam Raja and other plant species
between each of the pots.
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Table 2 : Germination rate for each pot.
NO.
|
POTS
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TIME
FOR FIRST SPROUT TO EMERGE
|
GERMINATION
RATE
|
|
DATE
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DURATION
(DAYS)
|
|||
01
|
Ground soil
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7/03/2018 - 23/04/2018
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47 days
|
Fast
|
02
|
Wet soil
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12/03/2018 - 23/04/2018
|
43 days
|
Moderate
|
03
|
Hill soil
|
No germination occur
|
||
04
|
Red soil
|
|||
05
|
Sand
|
5.0 DISCUSSION
After the eight weeks of
observation, the plant in ground soil shows the best germination out of four
other type of soils. However, there is only 1 out of 18 seeds that germinate in
the ground soil. The height of plant during 8th week is 23cm, the
length of root is 21.5cm while there is 2 other type of plant also germinate in
this soil. However, the seed that germinate in this soil grew around the pot
not in the middle. This is because the pot was too small and the root of this
plant is too long. No fauna found in the ground soil. Besides that, the number
of seeds that germinate in the wetland are three. The height of plants is 9cm,
6.5cm and 6.3cm respectively. The length of root are 21.5cm, 13.1cm and 19.0cm.
The plants in wetland slowly germinate, it is because of other plant grew in
this soil that might cause the competition between the plants. There also no
fauna found in the soil. Meanwhile, there are no germination of seeds in hill
soil, sand soil and red soil. But, there are two other plants that grew in hill
soil while one type of plant grew in red soil. No fauna were found in this three
type of soils also.
Theoretically, the soil texture can be tested by a few
methods such as test soil jar test and sieve analysis test. The result of soil
jar test and sieve analysis needed to compare to analyse soil texture to come
out with more precise result. From the soil jar, the most bottom layer shows
that the soil texture is sand while from the sieve analysis test, the soil that
remain in the pan and have passes through all the different six of sieve
opening mesh size are actually the silt and clay soil. The ground soil, hill
soil, red soil, wetland and sand showthe layer of sandy soil is thicker than
silt soil and clay soil. On top of that, based on result from sieve analysis,
it shows that there are only 3% to 9% of soil are silt and clay. The most
precision method to distinguish between silt texture and clay texture are by
using hydrometer analysis. From the sieve analysis shows that sand soil have
the lowest weight of soil remain in the pan as it explained that the sand
contain more sand soil than silt and clay soil. While for the jar test, the
layer of sand that can be seen are only one layer which is sand soil layer
because the layer of silt and clay soil are very thin as it cannot be
calculated. Hill soil contains the most soil remain in the pan but there are
only two layers in the jar test. This error can be occur as hill soil is either
have more silt soil or clay soil, so the lower the soil texture contain in the
soil, the thinner the layer it can be. The experiment that have been conducted
can only distinguish a bigger particle in size such as sand soil texture, while
further analysis such as hydrometer analysis need to conduct to distinguish a
smaller particle.
Soils host a complex web of organisms which can influence soil evolution and specific soil moisture and texture properties. For instance, earthworms activity increases infiltration rate, or microbial activity decreases soil organic matter due to mineralization. Soil biological properties are also interconnected with other soil moisture and texture properties. For example aeration, soil organic matter or pH affect the activity of many microorganisms in soils which in turn perform relevant activities in carbon and nutrients cycling. Thus, changes in soil properties due to management can significantly affect biological properties in soils, some of them being extremely sensitive to soil management. For example, soil microbial activity can be greatly increased by improved drainage, liming or organic amendments. That is why some soil biological properties can be used as indirect indicators of appropriate soil management and good soil quality, like soil respiration rate or some enzymatic activities that can be derived from living organisms in soil. Soil organic matter is a key factor affecting biological activity in soils. It is the carbon source for many organisms, including soil microbiota. Not only the amount, but also the type of organic compounds in the soil determines its biological activity. For example, microbial activity is greatly increased by incorporating fresh organic residues (such as green manure or crop residues), which can be readily mineralized by microbes.
The rhizosphere is the volume of soil altered by the root system and is the part of the soil profile where the concentration of suitable carbon sources for many microorganisms is greatest. Organic compounds exuded by plant roots (including organic anions of low molecular weight) alter soil chemical properties and greatly increase the biological activity in comparison to the bulk soil. The rhizosphere is a space of intense interaction of plant roots with soil microorganisms. Rhizospheric microorganisms can significantly affect plant development through the production of growth regulators, by decreasing the incidence of plant diseases, and by increasing nutrient availability to plants. Understanding soil biological properties is important for soil management but also for prevention and control of crop pests and diseases.
Soils host a complex web of organisms which can influence soil evolution and specific soil moisture and texture properties. For instance, earthworms activity increases infiltration rate, or microbial activity decreases soil organic matter due to mineralization. Soil biological properties are also interconnected with other soil moisture and texture properties. For example aeration, soil organic matter or pH affect the activity of many microorganisms in soils which in turn perform relevant activities in carbon and nutrients cycling. Thus, changes in soil properties due to management can significantly affect biological properties in soils, some of them being extremely sensitive to soil management. For example, soil microbial activity can be greatly increased by improved drainage, liming or organic amendments. That is why some soil biological properties can be used as indirect indicators of appropriate soil management and good soil quality, like soil respiration rate or some enzymatic activities that can be derived from living organisms in soil. Soil organic matter is a key factor affecting biological activity in soils. It is the carbon source for many organisms, including soil microbiota. Not only the amount, but also the type of organic compounds in the soil determines its biological activity. For example, microbial activity is greatly increased by incorporating fresh organic residues (such as green manure or crop residues), which can be readily mineralized by microbes.
The rhizosphere is the volume of soil altered by the root system and is the part of the soil profile where the concentration of suitable carbon sources for many microorganisms is greatest. Organic compounds exuded by plant roots (including organic anions of low molecular weight) alter soil chemical properties and greatly increase the biological activity in comparison to the bulk soil. The rhizosphere is a space of intense interaction of plant roots with soil microorganisms. Rhizospheric microorganisms can significantly affect plant development through the production of growth regulators, by decreasing the incidence of plant diseases, and by increasing nutrient availability to plants. Understanding soil biological properties is important for soil management but also for prevention and control of crop pests and diseases.
6.0 CONCLUSION
In
conclusion, what we can observed after 8 weeks of planting Cosmos
caudatus, among the
five types of soil, the most suitable soil to plant this type of plant is
ground soil and wet soil. The
growth rate of Cosmos caudatus are
faster in ground soil compare to wet soil. While theres are no germination
occur in hill soil, red soil and sand. Among the five types of soil, there are
another species growth inside the pot other than Cosmos caudatus except for sand soil. This is because sand soil
hold higher drainage system, so that all the nutrients did not hold inside the
soil. As for the ground soil, it hold the most nutrient content among the other
soil, so the plant can growth faster as it receive enough nutrient, water and
have a suitable pH for it to growth. Besides, the ground soil have a slower
rate of permeability compare to others, so the water and nutrient hold inside
the soil turns it to become the most suitable soil for the Cosmos caudatus to growth. As sand soil have high heavy metal
affect from its environment which can cause the availability of plant to grow
is lower than other soil. In a nutshell, in order for the Cosmos caudatus to grow, it need a soil with suitable pH value
which is in a range of 5.5 to 7.5. The soil texture are silt loam to growth the
Cosmos caudatus plant. As it also
need an enough nutrient and moisture content for the plant growth faster and
healthier.
REFERENCES
1.
Lumen
boundless biology. Nutritional Requirements of Plants. Access on 20 april 2018.
https://courses.lumenlearning.com/boundless-biology/chapter/nutritional-requirements-of-plants/
2.
T.K.
Hartz.2007.Soil Testing for Nutrient Availability Procedures and Interpretation
for California Vegetable Crop Production. Access on 20 April 2018.
4.
Potash
Development Association. 2011. Soil analysis: key to nutrient management
planning. Access on 21 April 2018 . https://www.pda.org.uk/pda_leaflets/24-soil-analysis-key-to-nutrient-management-planning/
5.
Royal
Horticultural Society. Nutrient deficiencies. https://www.rhs.org.uk/advice/profile?PID=456
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