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    Culture Media

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    and enriched media: EMB‚ blood and starch agar. OBJECTIVES: distinguish between different bacterial species based on colony morphology on agar plates To distinguish the growth characteristics of microorganisms in various differential‚ and selective media. Differentiate bacteria based on their ability to hydrolyze starch. Materials: Plates of EMB‚ Starch and blood agar. Stool sample. Inoculating loop. Bunsen burner. Soil sample. Cotton soap. Skin sample. Gram iodine. Results:

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    FLOW MEASUREMENT (Venturi meter‚ Orifice Plate and Rotameter) OBJECTIVES To study the characteristics and applications of various flow measuring device (venturi meter & orifice plate). To calculate the volume flow rate of water from the pressure difference of both venturi and orifice devices. To compare between theoretical and actual volumetric flow rate through the discharge coefficient concept. To know how rotameter works. INTRODUCTION The measurement of fluid flow is important in applications

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    ocean notes

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    The Mid-Atlantic Ridge‚ East Pacific Rise‚ East Africa Rift Valleys‚ Red Sea‚ Gulf of California are examples of what kind of plate boundaries. -divergent Andes Mountains‚ Cascade Mountains‚ Aleutian Islands‚ Mariana Islands‚ Himalaya Mountains‚ and the Alps are examples of what kind of plate boundaries -convergent Is it a faster or slower spreading mid-ocean ridge that produces broader and less rugged segments? -faster When you have Oceanic-Contintental convergance‚ which one

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    I will discus the history of earthquakes‚ the kinds and locations of earthquakes‚ earthquake effects‚ intensity scales‚ prediction‚ and my own predictions. An earthquake can be defined as vibrations produced in the earth’s crust. Tectonic plates have friction between them which builds up as it tries to push away and suddenly ruptures and then rebounds. The vibrations can range from barely noticeable to a disastrous‚ and destructive act of nature. Six kinds of shock waves are generated

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    seismic activity caused by the build-up of tension at the three types of plate boundaries: destructive‚ constructive and conservative. The pressure is suddenly released as the plates jerk past each other‚ sending out seismic waves from the focus that travel through different parts of the earth. The movement of convection currents within the Earth’s mantle causing the crust to become mobile which creates the different types plate margins‚ makes the cause due to physical factors. However human activity

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    IGCSE Geography

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    GCSE Geography Nicholas Rowles Series Editor: Jayne de Courcy PerfectBound An e-book from HarperCollins Publishers 77–85 Fulham Palace Road Hammersmith‚ London W6 8JB First published 2001 © HarperCollinsPublishers Ltd‚ 2001 Nicholas Rowles asserts the moral right to be identified as the author of this work Acrobat eBook Reader edition v 1. April 2001 ISBN: 0-00-712985-8 All rights reserved. You have been granted a non-exclusive‚ nontransferable licence to access and read the text

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    Gondwana: Nothofagus or Southern Beech.  A genus of around 40 extant species of trees. 3. Describe the theory of plate tectonics and identify its role in the formation of Australia as an island continent: The theory of plate tectonics states that Earth’s crust and the outermost part of the mantle are mechanically connected to each other. This layer is broken into several plates that move about Earth’s surface. As they move about‚ they are constantly interacting with each other along their boundaries

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    Copper Porphyry

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    There are four major factors that often contribute to the formation of hydrothermal copper porphyry: 1) readily available mineralizing fluid solutions that dissolve and transport metals‚ 2) openings in rocks which allow permeable flow of hydrothermal fluids and the metals that they transport in solution‚ 3) available sites within the fractured rocks which allow for deposition of the minerals from solution‚ and 4) the requisite chemical reactions that contribute to that deposition (Bateman‚ 1967)

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    Over time plate movement or subduction causes increasing strain on "sticking points" within the crust. Similar to if you rub two pieces of sand paper together‚ they will initially resist sliding until enough strain is built up. At that point‚ the "sticking point" is weakened and releases the built up strain. Before this theory was developed‚ scientists were unsure whether earthquakes caused faulting (plate movement) of faulting caused earthquakes. Today‚ over

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    suspension of T4 bacteriophages with a titer of at least 10‚000 phages/ml • 5 trypticase soy agar (TSA) plates. These should be warmed to 37c before use • 5 tubes of soft agar (0.7% agar). Prior to use‚ melt and hold at 50c in a water bath • 5 tubes of 9.0 ml trypticase soy (TS) broth • 1 ml sterile pipettes • Pipette aids Methods: 1. We began the experiment by marking the plates and place them in order from 10^5‚ 10^6‚ 10^7‚ then have the blank dilutions ready in order from 10^-4‚ 10^-5

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