BIOL 221 – Concepts of Botany Topic 12: Water Relations, Osmosis and Transpiration
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Conceptual Understanding of Osmosis and Diffusion by Australian First-Year Biology Students
International Journal of Innovation in Science and Mathematics Education, 27(9), 17-33, 2019 Conceptual Understanding of Osmosis and Diffusion by Australian First-year Biology Students Nicole B. Reinkea, Mary Kynna and Ann L. Parkinsona Corresponding author: Nicole B. Reinke ([email protected]) aSchool of Health and Sport Sciences, University of the Sunshine Coast, Sippy Downs QLD 4576, Australia Keywords: biology, osmosis, diffusion, conceptual assessment, misconception Abstract Osmosis and diffusion are essential foundation concepts for first-year biology students as they are a key to understanding much of the biology curriculum. However, mastering these concepts can be challenging due to their interdisciplinary and abstract nature. Even at their simplest level, osmosis and diffusion require the learner to imagine processes they cannot see. In addition, many students begin university with flawed beliefs about these two concepts which will impede learning in related areas. The aim of this study was to explore misconceptions around osmosis and diffusion held by first-year cell biology students at an Australian regional university. The 18- item Osmosis and Diffusion Conceptual Assessment was completed by 767 students. From the results, four key misconceptions were identified: approximately half of the participants believed dissolved substances will eventually settle out of a solution; approximately one quarter thought that water will always reach equal levels; one quarter believed that all things expand and contract with temperature; and nearly one third of students believed molecules only move with the addition of external force. Greater attention to identifying and rectifying common misconceptions when teaching first-year students will improve their conceptual understanding of these concepts and benefit their learning in subsequent science subjects. -
Circle Reverse Osmosis System
CIRCLE REVERSE OSMOSIS SYSTEM KEY FEATURES Water Saving Technology – Patented technology eliminates backpressure The RC100 conforms to common in conventional RO systems making the Circle up to 10 times more NSF/ANSI 42, 53 and efficient than existing products. 58 for the reduction of Saves You Money – Conventional RO systems waste up to 24 gallons of Aesthetic Chlorine, Taste water per every 1 gallon of filtered water produced. The Circle only wastes and Odor, Cyst, VOCs, an average of 2.1 gallons of water per 1 gallon of filtered water produced, Fluoride, Pentavalent Arsenic, Barium, Radium 226/228, Cadmium, Hexavalent saving you water and money over the life of the product!. Chromium, Trivalent Chromium, Lead, RO Filter Auto Flushing – Significantly extends life of RO filter. Copper, Selenium and TDS as verified Chrome Faucet Included – With integrated LED filter change indicator. and substantiated by test data. The RC100 conforms to NSF/ANSI 372 for Space Saving Compact Design – Integrated rapid refill tank means more low lead compliance. space under the sink. SPECIFICATIONS Product Name H2O+ Circle Reverse Osmosis Water Filtration System Model / SKU RC100 Installation Undercounter Sediment Filter, Pre-Carbon Plus Filter, Post Carbon Block Filter (RF-20): 6 months Filters & Lifespan RO Membrane Filter (RF-40): 24 months Tank Capacity 6 Liters (refills fully in less than one hour) Dimensions 9.25” (W) x 16.5” (H) x 13.75” (D) Net weight 14.6 lbs Min/Max Operating Pressure 40 psi – 120 psi (275Kpa – 827Kpa) Min/Max Water Feed Temp 41º F – 95º F (5º C – 35º C) Faucet Flow Rate 0.26 – 0.37 gallons per minute (gpm) at incoming water pressure of 20–100 psi Rated Service Flow 0.07 gallons per minute (gpm) Warranty One Year Warranty PO Box 470085, San Francisco CA, 94147–0085 brondell.com 888-542-3355. -
Master Gardener PUBLISHED by UNIVERSITY of MISSOURI EXTENSION Extension.Missouri.Edu
Master Gardener PUBLISHED BY UNIVERSITY OF MISSOURI EXTENSION extension.missouri.edu Plants and Their Environment David Trinklein, Division of Plant Sciences lants are living organisms that contain chlorophyll and use it to manufacture Ptheir own food. Their cell walls are more or less rigid and support both the individual cells and the whole structure. Even when plants have reached what we regard as their full, mature size, they continue to expand and develop new leaves, flowers, fruit and shoots. Unlike animals, plants cannot move when the environment changes. They are at the mercy of the climate and the gardener because they are rooted in place. Even though it appears that many plants, especially larger ones, are quite tolerant of change, they sometimes do not show adverse effects until long after the event. For example, tree roots are often damaged or killed by suffocation during building projects or flooding. An established tree may still have strength to leaf out and may appear to thrive for several years. But in its weakened state, the tree is more likely to blow down, become infested or simply decline. To understand why plants respond as they do to natural influences and to cultivation, gardeners must understand something about their structure and how they grow. This publication provides such an introduction. Ways to group plants Uses Gardeners tend to group plants by their horticultural uses: fruits, vegetables, flowers, trees, shrubs, turf and so on. These categories are a convenient way to think and learn about plants. Life cycle Plants can also be categorized by the length of their life cycles. -
Evaluation of the Osmotic Adjustment Response Within the Genus Beta
July 2008 - Dec. 2008 Osmotic Adjustment Response 119 Evaluation of the Osmotic Adjustment Response within the Genus Beta Manuela Bagatta, Daniela Pacifico, and Giuseppe Mandolino C.R.A. – Centro di Ricerca per le Colture Industriali Via di Corticella 133 – 40128 Bologna (Italy) Corresponding author: Giuseppe Mandolino ([email protected]) ABSTRACT Beta genus includes both industrial and horticultural spe- cies, and wild species and subspecies, which are possible reservoirs of agronomically important characters. Among the traits for which Beta has been recently studied, drought tolerance or avoidance is one of the most important. In this work, relative water content and the osmotic potential in well-watered and stressed conditions of three beet types, one B. vulgaris subspecies and one species other than B. vulgaris, all belonging to the Beta genus, were analysed. In addition, relative water content, succulence index and osmotic potential were measured during a three-week water deprivation period, and the osmotic adjustment was estimated for each Beta accession. The results showed that succulence was higher for B. vulgaris ssp. maritima. It was also shown that all Beta accessions were capable of adjust- ing osmotically, but that the B. vulgaris maritima accession examined had a higher osmotic adjustment value compared to the accessions belonging to cultivated Beta types, and that the accession of the wild species Beta webbiana had a comparatively limited capacity to adjust osmotically. Additional key words: Sugarbeet, sea beet, germplasm, drought, osmotic adjustment rought is one of the greatest limitations for agriculture and crop expansion (Boyer, 1982). Sugarbeet (Beta vulgaris ssp. vulgaris) is aD deep-rooting crop, more adapted to withstand water shortage or nutri- tional deprivation than many other crops (Doorenbos and Kassam, 1979; Biancardi et al., 1998); however, drought stress is becoming a major 120 Journal of Sugar Beet Research Vol. -
The New Formula That Replaces Van't Hoff Osmotic Pressure Equation
New Osmosis Law and Theory: the New Formula that Replaces van’t Hoff Osmotic Pressure Equation Hung-Chung Huang, Rongqing Xie* Department of Neurosciences, University of Texas Southwestern Medical Center, Dallas, TX *Chemistry Department, Zhengzhou Normal College, University of Zhengzhou City in Henan Province Cheng Beiqu excellence Street, Zip code: 450044 E-mail: [email protected] (for English communication) or [email protected] (for Chinese communication) Preamble van't Hoff, a world-renowned scientist, studied and worked on the osmotic pressure and chemical dynamics research to win the first Nobel Prize in Chemistry. For more than a century, his osmotic pressure formula has been written in the physical chemistry textbooks around the world and has been generally considered to be "impeccable" classical theory. But after years of research authors found that van’t Hoff osmotic pressure formula cannot correctly and perfectly explain the osmosis process. Because of this, the authors abstract a new concept for the osmotic force and osmotic law, and theoretically derived an equation of a curve to describe the osmotic pressure formula. The data curve from this formula is consistent with and matches the empirical figure plotted linearly based on large amounts of experimental values. This new formula (equation for a curved relationship) can overcome the drawback and incompleteness of the traditional osmotic pressure formula that can only describe a straight-line relationship. 1 Abstract This article derived a new abstract concept from the osmotic process and concluded it via "osmotic force" with a new law -- "osmotic law". The "osmotic law" describes that, in an osmotic system, osmolyte moves osmotically from the side with higher "osmotic force" to the side with lower "osmotic force". -
Osmosis and Osmoregulation Robert Alpern, M.D
Osmosis and Osmoregulation Robert Alpern, M.D. Southwestern Medical School Water Transport Across Semipermeable Membranes • In a dilute solution, ∆ Τ∆ Jv = Lp ( P - R CS ) • Jv - volume or water flux • Lp - hydraulic conductivity or permeability • ∆P - hydrostatic pressure gradient • R - gas constant • T - absolute temperature (Kelvin) • ∆Cs - solute concentration gradient Osmotic Pressure • If Jv = 0, then ∆ ∆ P = RT Cs van’t Hoff equation ∆Π ∆ = RT Cs Osmotic pressure • ∆Π is not a pressure, but is an expression of a difference in water concentration across a membrane. Osmolality ∆Π Σ ∆ • = RT Cs • Osmolarity - solute particles/liter of water • Osmolality - solute particles/kg of water Σ Osmolality = asCs • Colligative property Pathways for Water Movement • Solubility-diffusion across lipid bilayers • Water pores or channels Concept of Effective Osmoles • Effective osmoles pull water. • Ineffective osmoles are membrane permeant, and do not pull water • Reflection coefficient (σ) - an index of the effectiveness of a solute in generating an osmotic driving force. ∆Π Σ σ ∆ = RT s Cs • Tonicity - the concentration of effective solutes; the ability of a solution to pull water across a biologic membrane. • Example: Ethanol can accumulate in body fluids at sufficiently high concentrations to increase osmolality by 1/3, but it does not cause water movement. Components of Extracellular Fluid Osmolality • The composition of the extracellular fluid is assessed by measuring plasma or serum composition. • Plasma osmolality ~ 290 mOsm/l Na salts 2 x 140 mOsm/l Glucose 5 mOsm/l Urea 5 mOsm/l • Therefore, clinically, physicians frequently refer to the plasma (or serum) Na concentration as an index of extracellular fluid osmolality and tonicity. -
Summary a Plant Is an Integrated System Which: 1
Summary A plant is an integrated system which: 1. Obtains water and nutrients from the soil. 2. Transports them 3. Combines the H2O with CO2 to make sugar. 4. Exports sugar to where it’s needed Today, we’ll start to go over how this occurs Transport in Plants – Outline I.I. PlantPlant waterwater needsneeds II.II. TransportTransport ofof waterwater andand mineralsminerals A.A. FromFrom SoilSoil intointo RootsRoots B.B. FromFrom RootsRoots toto leavesleaves C.C. StomataStomata andand transpirationtranspiration WhyWhy dodo plantsplants needneed soso muchmuch water?water? TheThe importanceimportance ofof waterwater potential,potential, pressure,pressure, solutessolutes andand osmosisosmosis inin movingmoving water…water… Transport in Plants 1.1. AnimalsAnimals havehave circulatorycirculatory systems.systems. 2.2. VascularVascular plantsplants havehave oneone wayway systems.systems. Transport in Plants •• OneOne wayway systems:systems: plantsplants needneed aa lotlot moremore waterwater thanthan samesame sizedsized animals.animals. •• AA sunflowersunflower plantplant “drinks”“drinks” andand “perspires”“perspires” 1717 timestimes asas muchmuch asas aa human,human, perper unitunit ofof mass.mass. Transport of water and minerals in Plants WaterWater isis goodgood forfor plants:plants: 1.1. UsedUsed withwith CO2CO2 inin photosynthesisphotosynthesis toto makemake “food”.“food”. 2.2. TheThe “blood”“blood” ofof plantsplants –– circulationcirculation (used(used toto movemove stuffstuff around).around). 3.3. EvaporativeEvaporative coolingcooling. -
What Is the Difference Between Osmosis and Diffusion?
What is the difference between osmosis and diffusion? Students are often asked to explain the similarities and differences between osmosis and diffusion or to compare and contrast the two forms of transport. To answer the question, you need to know the definitions of osmosis and diffusion and really understand what they mean. Osmosis And Diffusion Definitions Osmosis: Osmosis is the movement of solvent particles across a semipermeable membrane from a dilute solution into a concentrated solution. The solvent moves to dilute the concentrated solution and equalize the concentration on both sides of the membrane. Diffusion: Diffusion is the movement of particles from an area of higher concentration to lower concentration. The overall effect is to equalize concentration throughout the medium. Osmosis And Diffusion Examples Examples of Osmosis: Examples of osmosis include red blood cells swelling up when exposed to fresh water and plant root hairs taking up water. To see an easy demonstration of osmosis, soak gummy candies in water. The gel of the candies acts as a semipermeable membrane. Examples of Diffusion: Examples of diffusion include perfume filling a whole room and the movement of small molecules across a cell membrane. One of the simplest demonstrations of diffusion is adding a drop of food coloring to water. Although other transport processes do occur, diffusion is the key player. Osmosis And Diffusion Similarities Osmosis and diffusion are related processes that display similarities. Both osmosis and diffusion equalize the concentration of two solutions. Both diffusion and osmosis are passive transport processes, which means they do not require any input of extra energy to occur. -
Introduction to Osmosis
DIFFUSION & OSMOSIS EXPLORE LAB SCIENCE WHAT IS DIFFUSION? Diffusion is the net movement of molecules from areas of high concentration to areas of low concentration of that molecule. This random movement, or Brownian motion, is the result of collisions with other molecules in the medium. To see diffusion in action, put a drop of food coloring into a glass of water and see how it behaves. GRADIENTS The movement of particles from high to low concentration is called “moving down the concentration gradient.” Low concentration High concentration EQUILIBRIUM Molecules will continue to diffuse like this until they reach equilibrium, or until there are equal concentrations of that molecule throughout the whole medium. This is why the food coloring particles disperse until the water is the same color all the way through. OSMOSIS Osmosis is a specialized type of diffusion that describes the movement of water molecules. Osmosis occurs when you have membrane with unequal concentrations of water molecules on either side. Water molecules will diffuse across the membrane until equilibrium is reached. SEMIPERMEABLE MEMBRANES When you made your naked eggs, you removed their shell. Now they are surrounded by a semipermeable membrane. What is let across the membrane is determined by the size, shape, or charge of the molecule and the characteristics of the membrane’s pores. The egg membrane is only permeable water in your experiments, so all the changes you see are because of the movement of water across the membrane. NAKED EGG EXPERIMENT If you put your naked egg in But if you put your egg in water, you probably noticed corn syrup or salt water, it that it got bigger. -
Transport of Water and Solutes in Plants
Transport of Water and Solutes in Plants Water and Solute Potential Water potential is the measure of potential energy in water and drives the movement of water through plants. LEARNING OBJECTIVES Describe the water and solute potential in plants Key Points Plants use water potential to transport water to the leaves so that photosynthesis can take place. Water potential is a measure of the potential energy in water as well as the difference between the potential in a given water sample and pure water. Water potential is represented by the equation Ψsystem = Ψtotal = Ψs + Ψp + Ψg + Ψm. Water always moves from the system with a higher water potential to the system with a lower water potential. Solute potential (Ψs) decreases with increasing solute concentration; a decrease in Ψs causes a decrease in the total water potential. The internal water potential of a plant cell is more negative than pure water; this causes water to move from the soil into plant roots via osmosis.. Key Terms solute potential: (osmotic potential) pressure which needs to be applied to a solution to prevent the inward flow of water across a semipermeable membrane transpiration: the loss of water by evaporation in terrestrial plants, especially through the stomata; accompanied by a corresponding uptake from the roots water potential: the potential energy of water per unit volume; designated by ψ Water Potential Plants are phenomenal hydraulic engineers. Using only the basic laws of physics and the simple manipulation of potential energy, plants can move water to the top of a 116-meter-tall tree. Plants can also use hydraulics to generate enough force to split rocks and buckle sidewalks. -
The Osmotic Adjustment of Marine Microalgae
The osmotic adjustment of marine microalgae and the complex role osmolytes play in this process Thesis of Liz Kendall Supervisor Dr. Gieskes Department of Marine Biology, The University of Groningen April 1996 D5O Summary: Algae inhabit a wide variety of both marine and freshwater habitats. These habitats differ in regard to various factors such as chemical composition, the organisms that live there, the light which may radiate into that particular area, the temperature of the sites depending on where the environment is located, just to name a few. One factor that varies from environment to environment is the salinity. This paper will look at the mechanisms utilized by marine algae to cope with the changes in salinity content in their habitats and most importantly how they use different osmolytes to carry out this process. Marine algae "osmotically adjust" themselves to external salinity changes, in a biphasic maimer. Firstly, this includes changes in turgor pressure or large internal water fluxes in response to osmotic gradients. Secondly. an internally regulated osmotic adjustment occurs with the use of both inorganic and organic osmolytes. Compatible solutes are ions and molecules used by man organisms to osmotically adjust and they play a double role in the process of osmotic adjustment. They act as osmolytes and also protect the cellular enzymatic activities under salinity stress. They are called 'compatible solutes" because they protect the cellular enzymatic activity. The main compatible solutes are polyols (including amino acids, carbohydrates and sugars). quaternary ammonium derivatives or tertiary sulphonium compounds. Certain species and taxonomic classes use specific compatible solutes and some even use combinations of them. -
Engineering Aspects of Reverse Osmosis Module Design
Lenntech [email protected] Tel. +31-152-610-900 www.lenntech.com Fax. +31-152-616-289 Engineering Aspects of Reverse Osmosis Module Design Authors: Jon Johnson +, Markus Busch ++ + Research Specialist, Research and Development, Dow Water & Process Solutions ++ Global Desalination Application Specialist, Dow Water & Process Solutions Email:[email protected] Abstract During the half century of development from a laboratory discovery to plants capable of producing up to half a million tons of desalinated seawater per day, Reverse Osmosis (RO) technology has undergone rapid transition. This transition process has caused signification transformation and consolidation in membrane chemistry, module design, and RO plant configuration and operation. From the early days, when cellulose acetate membranes were used in hollow fiber module configuration, technology has transitioned to thin film composite polyamide flat-sheet membranes in a spiral wound configuration. Early elements – about 4-inches in diameter during the early 70s – displayed flow rates approaching 250 L/h and sodium chloride rejection of about 98.5 percent. One of today’s 16-inch diameter elements is capable of delivering 15-30 times more permeate (4000-8000 L/h) with 5 to 8 times less salt passage (hence a rejection rate of 99.7 percent or higher). This paper focuses on the transition process in RO module configuration, and how it helped to achieve these performance improvements. An introduction is provided to the two main module configurations present in the early days, hollow fiber and spiral wound and the convergence to spiral wound designs is described as well. The development and current state of the art of the spiral wound element is then reviewed in more detail, focusing on membrane properties (briefly), membrane sheet placement (sheet length and quantity), the changes in materials used (e.g.