MINI PROJECT: TARAB ARAB PADI SAWAH

CAPTAIN: Ng Jing Jie
Mohamed Fickry
Marilyn Leanne Monroe
Nurul Irina
Siti Nurazwanni
Emiley 

 Report Submission:
First Lab Report (Link)
Second Lab Report (Link)
Third Lab Report (Link)
Fourth Lab Report (Link)
Fifth Lab Report (Link)
Hardcopy Overall Summary Report

Lab Schedule:
26th March 2018 - Soil permeability Test (Click Here)
26th March 2018 - Sieve Analysis Test (CLICK HERE)
9th April 2018 - Soil Salinity Test (CLICK HERE)
23rd April 2018- Soil Nutrient Analysis (CLICK HERE)

 Research Questions:
  1. Among each soil which is the most suitable soil to grow Paddy?
  2. How does moisture content of each soil affect the Paddy growth?
  3. Which soil is most fertile to grow Paddy productively?
  4. How does the growth of Paddy related with soil minerals and phytoavailability/bioavailabilty?
  5. How does soil moisture and soil texture affect soil biology: rhizosphere activities/interaction?
Materials:
  1. Paddy seeds
  2. 5 pots (No hole, need to keep water)
  3. 500ml recycle bottle (for watering)
  4. 5 different soil texture (each soil sample can fit 2 pots, one portion for soil medium and one for lab analysis (record GPS soil sample location taken, can upload apps from smartphone)
  5. 5 recycle empty transparent bottle glass jar for soil texture analysis (same size, smooth even surface).
  6. 5 empty recycle tin can (same size), poke same number of holes at the bottom of the can.
  7. 10 Recycle plastic container for air-dry soil.
  8. Camera/video (smartphone). Record paddy growth development.
1st Lab Analysis (Report submit online due 20th March 2018):

  1. Fill up the pot 2/3 with soil. Pat the soil to compress the soil so that the level of soil does not shrink after watering.
  2. Divide the number of seeds equally for each pot and space the seeds when seed sowing.
  3. Top about 2cm thick of soil after seed are placed on the soil. Then water with same amount (500ml) for each pot.
  4. Soil Color Analysis.
  5. Soil Texture Analysis.
  6. Soil Moisture: Weight 100 gram of each type of soil, record. Then air-dry soil. After 2 weeks if soil have no more moisture, weight dry soil.
  7. Water the soil two times a week until 26th March 2018. The watering frequency change after 26th March 2018.
    Observation Record:
    1. Germination rate for each pot.
    2. Mortality/survival rate of the plant growth.
    3. How long does seeds start to sprout an emerge from the soil for each soil texture.
    4. Average growth of the plants (root, shoot and whole plant) for each soil texture every two weeks.
    5. Nutrient availability of each soil sample.
    6. Deficiency symptoms.
    7. Capture photos of the plant development.
    Watering Frequency and Growth Monitoring:

    5th March - 26th March 2018 : Water two times a week same amount.

    26th March 2018 - 23rd April 2018 : Water once a  week.

    23rd April 2018 : Dug out carefully 3 plants (make sure roots intact) from each pot and measure the length of root, shoot and whole plant. Measure the wet weight of the whole plant. Then dry the plant, after plant dried completely. Measure plant dry weight.

    SUGGESTION:

    Read up on Paddy.

    Get to know how to grow Paddy, its like and dislike.

    Don't forget to keep your reference list for your report. Citations.

    Fill free to add on research questions or observation data. 

    Comments

    Post a Comment

    Popular posts from this blog

    First Lab Report: Cotton

    Image
    1) Soil Texture INTRODUCTION Soil is a material composed of five ingredients — minerals, soil organic matter, living organisms, gas, and water (Needelman, 2013). Soil performs many essential functions in almost any ecosystems, like farm, forest, marsh and so on. Soil is a natural resource, an amazing substance. Earth is unique because there is dirt on Earth, Mars and Venus do not have soil. The texture and the distribution of mineral particles in the soil are the most important for the soil. Soil texture is an inherent soil quality property (Measuring Soil Texture in the Laboratory, 2018). The percentages of particles in these size classes is called soil texture (Needelman, 2013). Soil texture affects microbial activity by directly affecting water content and the temperature of soil (Chodak et al., 2010). The textural class is also important for soil aggregation and porosity. In addition, soil texture plays a key role in gas exchange (respiration of roots and microor
    Read more

    Lab Report 2 : Sengkuang

    Image
    Second Lab Report : Sengkuang Lecturer: Mdm. Diana Demiyah Mohd Hamdan Group Members : 1.0  INTRODUCTION      Water holding capacity designates the ability of a soil to hold water. It is useful information for irrigation scheduling, crop selection, groundwater contamination considerations, estimating runoff and determining when plants will become stressed. Soil moisture available for plant growth makes up approximately 0.01 percent of the world's stored water. Soil texture and structure greatly influence water infiltration, permeability and water-holding capacity. Soil texture refers to the composition of the soil in terms of the proportion of small, medium and large particles (clay, silt, and sand, respectively) in a specific soil mass. For example, a coarse soil is sand or loamy sand, a medium soil is a loam, silt loam, or silt and a fine soil is a sandy clay, silt clay, or clay. Water holding capacity varies by soil texture.      Soil moisture
    Read more

    First Lab Report: JAGUNG PANDAN (Analysis of Soil Colour and Soil Texture)

    Image
    Title: Soil Colour and Soil Texture Analysis Lecturer: Dr. Diana Demiyah Mohd Hamdan Date of Submission: 24th March 2018 NAME MATRIC NUMBER SOW XIAO HUI BS17110464 KONG WAN LING BS17110429 AARON CHIN VUI CHANG BS17160670 NURUL NATASYAH BINTI KANAPIA@HANAFIAH BS17110546 NURFATIN SOFEA BINTI MOHD HELMI BS17110574 Soil Colour Analysis 1.0 Introduction The colour of the soil is usually the first thing people notice. Mostly this is just the topsoil but it does not reflect the entire soil. The topsoil is usually darker than lower layers (or horizons) because this is where organic matter accumulates. Soil colour is usually due to 3 main pigments: black—from organic matter, red—from iron and aluminium oxides and white—from silicates and salt. Colour can be a useful indicator of some of the general properties of a soil, as well as some of the chemical processes that are occu
    Read more