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Adsorption Isotherms
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Mechanism of Absorption of Elements

Last Updated : 07 Jun, 2024
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The mechanism of absorption of elements in plants involves the absorption of mineral elements from the soil and transporting them to different plant parts. This mechanism of absorption of elements or minerals by plants includes two phases: passive absorption and active absorption

The roots actively take up these minerals through specialized cells and translocate them to other plant parts. In this article, we will study the mechanism of absorption of elements in detail.

Table of Content

  • Essential Elements and Mineral Absorption
  • Mechanism of Absorption of Elements
  • Passive Absorption of Elements
    • Mass Flow Hypothesis
    • Simple Diffusion Hypothesis
    • Facilitated Diffusion
    • Ion Exchange Hypothesis
      • Contact Exchange Theory
      • Carbonic Acid Exchange Theory
    • Donnan Equilibrium
  • Active Absorption
  • Difference Between Passive and Active Absorption
  • Factors Affecting Mechanism of Absorption of Elements

Essential Elements and Mineral Absorption

Essential elements are nutrients required by plants in specific amounts for proper growth, development, and physiological functions. These elements are directly involved in plant metabolism and cannot be replaced. This shows how important they are for plants in their life cycle.

These mineral elements are found scattered in the soil. Plants absorb essential elements from the soil through their roots, utilizing both active transport and passive diffusion. Root hairs increase the surface area for nutrient uptake, and once absorbed, these elements are transported through the xylem to various parts of the plant. Soil composition and pH significantly influence the efficiency of this absorption process.

Regions-of-root
Region of Root

Classification of Elements

Mineral elements are classified into two main groups based on the quantity required by plants:

  • Macronutrients: These are needed in large amounts and include elements like nitrogen, phosphorus, and potassium. They are essential for basic plant functions and growth.
  • Micronutrients: Required in smaller quantities, micronutrients include elements like iron, zinc, and manganese. Despite their lower quantity, they are crucial for specific metabolic processes in plants.

Also Read: Difference Between Micronutrients and Macronutrients

Mechanism of Absorption of Elements

Minerals are taken up by plants either in their dissolved form or from the soil. This absorption occurs in the cells of the epiblema located in the root zones of maturation and elongation. The process of mineral absorption happens in two main phases:

  • Passive Absorption
  • Active Absorption

Now, let's study each of them in detail.

Passive Absorption of Elements

Passive absorption of mineral elements occurs without the expenditure of energy. Here, they rely on natural physical processes to move minerals into plant roots. This process is driven by the concentration gradients and other physical forces. The following hypotheses and mechanisms explain the passive absorption of minerals:

Mass Flow Hypothesis

According to mass flow hypothesis, minerals are transported to the roots along with the flow of water during transpiration. As water is absorbed by the roots and pulled upwards through the plant, it carries dissolved minerals with it. This process ensures a continuous supply of nutrients as long as the transpiration stream is active.

Also Read: The Pressure Flow or Mass Flow Hypothesis

mass_flow_hypothesis_50
Mass Flow Hypothesis

Simple Diffusion Hypothesis

Simple diffusion involves the movement of mineral ions from an area of higher concentration in the soil solution to an area of lower concentration inside the root cells. This process is driven purely by the concentration gradient of the ions, without the involvement of energy or transporter proteins.

Facilitated Diffusion

Unlike simple diffusion, facilitated diffusion requires specific carrier proteins or channels in the cell membrane to help the movement of ions. These proteins help transport ions that cannot diffuse freely across the lipid bilayer, making the process more efficient and selective.

Facilitated-Diffusion
Facilitated Diffusion

Also Read: What is Facilitated Diffusion?

Ion Exchange Hypothesis

In this hypothesis, the absorption of mineral ions occurs through the exchange of ions between the soil particles and the root surface. Here are two key theories that explain this process:

Contact Exchange Theory

  • Mechanism: Ions are exchanged through direct contact between the root surface and soil particles.
  • Cation Exchange: For example, potassium ions (K+) from the soil solution are exchanged with hydrogen ions (H+) absorbed on the root surface membrane.
  • Anion Exchange: Similarly, anions in the soil can be exchanged with hydroxyl ions (OH-) from the root.
  • Dynamic Movement: Ions are not tightly bound to soil particles (clay micelles) but can move within a small volume of space.
  • Electrostatic Absorption: Ions are absorbed electrostatically to the plant root and exchanged with ions held by the clay micelles.
  • Diffusion: The exchanged cations and anions are then moved into the roots by simple diffusion.

Carbonic Acid Exchange Theory

  • Mechanism: Ions are exchanged in their dissolved form in the soil solution.
  • Formation of Carbonic Acid: Carbon dioxide released during respiration combines with water to form carbonic acid in the soil solution.
  • Dissociation: Carbonic acid dissociates into hydrogen ions (H+) and bicarbonate ions (HCO3-).
  • Cation Exchange: Hydrogen ions replace cations adsorbed on clay particles, releasing these cations into the soil solution.
  • Anion Exchange: Bicarbonate ions release adsorbed anions, supplying both anions and cations to the plant roots.

Donnan Equilibrium

This concept, introduced by F.G. Donnan, highlights the passive accumulation of non-diffusible particles against the electrical potential gradient (ECP) angle. The cellular membrane selectively allows the passage of diffusible particles, while non-diffusible particles called fixed particles, remain constrained.

These fixed particles, which can be either anions or cations, are predominantly present on one side of the membrane, forming the Donnan phase. According to Donnan's equilibrium principle, ions of opposite charge are attracted to balance the charge of fixed particles:

  • If anions serve as non-diffusible fixed particles, cations of corresponding charge are absorbed.
  • If cations serve as fixed particles, anions of corresponding charge are absorbed.

The Donnan equilibrium can be mathematically described by the following equation.

[Ci+] [Ai-] = [Co+] [Ao-]

Where Ci+ = Cations inside
Co+ = Cations outside
Ai- = Anion inside
Ao-= Anion outside

Active Absorption of Elements

Active absorption of mineral elements in plants involves the utilization of energy to transport ions against their concentration gradient, ensuring the uptake of essential nutrients even when they are scarce in the soil. This process is crucial for maintaining optimal levels of nutrients within the plant. Here's how active absorption works:

  • ATP-Dependent: Active absorption relies on adenosine triphosphate (ATP) for energy, enabling carrier proteins to transport ions against their concentration gradient.
  • Ion Channels and Pumps: Carrier proteins in the cell membrane facilitate selective transport of ions, ensuring only specific ions pass through.
  • Uptake of Scarce Nutrients: Active absorption allows plants to absorb mineral ions from the soil even when their concentration is lower outside root cells.
  • Controlled Process: The activity of carrier proteins is regulated by factors such as metabolic status, hormonal signals, and environmental conditions.
  • Selective Uptake: Carrier proteins exhibit specificity for particular ions, allowing plants to absorb essential nutrients efficiently while excluding harmful ions.

Difference Between Passive and Active Absorption

The difference between passive and active absorption is given below:

Feature

Passive Absorption

Active Absorption

Energy Requirement

Does not require energy; occurs spontaneously

Requires energy (ATP) for ion transport against concentration gradient

Type of Transport

Simple diffusion, facilitated diffusion, mass flow

Carrier-mediated transport using specific proteins

Direction of Movement

Along concentration gradient

Against concentration gradient

Regulation

Not actively regulated; dependent on external factors

Actively regulated by cellular processes and signals

Selectivity

Less selective; allows movement of ions based on concentration gradient

Highly selective; specific carrier proteins allow uptake of particular ions

Examples

Movement of water and ions through cell membrane

Uptake of scarce nutrients like potassium and iron

Factors Affecting Mechanism of Absorption of Elements

The factors affecting are:

  • Soil pH: Soil pH influences the availability of mineral ions and their solubility, affecting their absorption by plant roots.
  • Soil Texture: Soil texture impacts water retention and the movement of mineral ions in the soil, influencing their accessibility to plant roots.
  • Soil Microorganisms: Microbial activity in the soil can enhance nutrient availability through processes like mineralization and nitrogen fixation.
  • Root Surface Area: The presence of root hairs and the extent of root branching affect the surface area available for nutrient absorption.
  • Root Health: The condition of plant roots, including their structure and health, can impact their ability to absorb nutrients effectively.
  • Environmental Factors: Factors such as temperature, moisture levels, and light intensity can influence nutrient uptake by affecting root metabolism and physiological processes.

Conclusion - Mechanism of Absorption of Elements

Essential elements are super important for plants because they help them grow, stay healthy, and do all kinds of important stuff in their bodies. These nutrients are found in the soil, and plants suck them up through their roots using different ways like active transport and passive diffusion. Root hairs help grab more nutrients from the soil, and then they travel up the plant through the xylem. The type of soil and how acidic or basic it is can affect how well plants can get these nutrients. By knowing how plants absorb nutrients, farmers can grow better crops and get more food from their fields.

Also Read:

  • Digestion and Absorption
  • Difference Between Absorption and Adsorption
  • How Do Plants Absorb Nutrients?

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Adsorption Isotherms

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    Elements with partially filled d orbitals are known as transition elements (sometimes known as transition metals). Transition elements are defined by IUPAC as elements with a partially full d subshell or elements capable of forming stable cations with an incompletely filled d orbital. In general, an
    7 min read
    Some Important Compounds of Transition Elements
    Transition metals are typically characterized as elements with or capable of forming partially filled 'd' orbitals. Transition elements are d-block elements in groupings of three to eleven. Inner transition metals, which include the lanthanides and actinides, are another name for the f block element
    6 min read
    Lanthanides - Definition, Configuration, Properties
    Lanthanides are the contemporary periodic table's rare earth elements, with atomic numbers ranging from 58 to 71 after Lanthanum. Rare earth metals are so-called because these elements are extremely rare (3 × 10-4 % of the Earth's crust). As lanthanide orthophosphates, they are accessible in 'monazi
    8 min read
    Actinides - Definition, Properties, Formation, Uses
    The d and f block mainly contains elements that include groups 3-12. The f block has elements in which 4f and 5f are progressively filled. These elements are placed below the periodic table in a separate table. The d and f block elements are majorly known as transition or inner transition elements.
    9 min read
    Some Applications of d and f-block Elements
    Transition metals are typically characterized as elements with or capable of forming partially filled 'd' orbitals. Transition elements are d-block elements in groupings of three to eleven. Inner transition metals, which include the lanthanides and actinides, are another name for the f block element
    6 min read

    Chapter 9 Coordination Compounds

    Werner's Theory
    Werner's Theory of Coordination Compounds was proposed by a Swiss Chemist Alfered Werener in 1898. Werner studied the physical, chemical, and isomeric properties of several coordination compounds and postulated some theories. In this article, we will learn about, Werner's Coordination theory, its po
    8 min read
    Important Terms pertaining to Coordination Compounds
    A coordination compound is made up of a central metal atom or ion that is surrounded by a number of oppositely charged ions or neutral molecules. All the ions or molecules in coordination compounds are connected with coordinate bonds to the central metal atom. When coordination compounds are dissolv
    6 min read
    Nomenclature of Coordination Compounds
    The ability of the transition metals to form the complexes is referred to as coordination compounds. This property is not only applicable to transition metal only but also shown by some other metals. Werner, in 1893 was the first scientist to propose the theory of coordination compounds and also pur
    10 min read
    Isomerism in Coordination Compounds
    Isomerism in Coordination Compounds as the name suggests explores the concept of Isomerism in Coordination Compounds i.e., generally compounds formed by d-block elements. Isomerism is the phenomenon of exhibiting different molecular structures by the compounds with same molecular formula. The phenom
    10 min read
    Valence Bond Theory in Coordination Compounds
    There have been numerous approaches proposed to explain the nature of bonding in coordination molecules. One of them is the Valence Bond (VB) Theory. The Valence Bond Theory was developed to describe chemical bonding using the quantum mechanics method. This theory is largely concerned with the produ
    9 min read
    Crystal Field Theory
    A coordination compound consists of a metal atom or ion at the centre, surrounded by a number of oppositely charged ions or neutral molecules. A coordinate connection connects these ions or molecules to the metal atom or ion. When dissolved in water, they do not dissociate into simple ions. Crystal
    7 min read
    Applications of Coordination Compounds
    Chemical compounds made up of an array of anions or neutral molecules linked to a central atom by coordinate covalent bonds are known as coordination compounds. Coordination compounds are also known as coordination complexes. Ligands are the molecules or ions that are bonded to the central atom (als
    7 min read

    Chapter 10 Haloalkanes and Haloarenes

    Haloalkanes and Haloarenes
    Haloalkanes and haloarenes are hydrocarbons that have had one or more hydrogen atoms replaced with halogen atoms. The major distinction between haloalkanes and haloarenes is that the former are formed from open-chain hydrocarbons (alkanes), whilst the latter are derived from aromatic hydrocarbons. H
    13 min read
    Methods of preparation of Haloalkanes and Haloarenes
    Alkyl halide (haloalkane) and aryl halide (haloarene) are formed when hydrogen atoms in an aliphatic or aromatic hydrocarbon are replaced by halogen atoms. Haloalkanes have halogen atom(s) attached to an alkyl group's sp3 hybridized carbon atom(s), whereas haloarenes have halogen atom(s) attached to
    5 min read
    Physical Properties of Haloalkanes and Haloarenes
    Haloalkanes and haloarenes are organic compounds formed when hydrogen atoms are replaced with halogen atoms in aliphatic or aromatic hydrocarbons. Haloalkanes and haloarenes are also called alkyl halide and aryl halide respectively. Haloalkanes and haloarenes organic compounds are found in nature an
    4 min read
    Chemical reactions of Haloalkanes and Haloarenes
    When a hydrogen atom in an aromatic or aliphatic hydrocarbon is replaced with a halogen atom, haloalkanes and haloarenes are produced. Haloalkanes are generated when an H-atom is replaced in an aliphatic hydrocarbon, whereas Haloarenes are formed when the same H-atom is replaced in an aromatic hydro
    8 min read
    Polyhalogen Compounds - Definition, Properties, Uses
    Hydrocarbons having one or more hydrogen atoms substituted by halogen atoms are known as haloalkanes and haloarenes. Haloalkanes and haloarenes are distinguished by the fact that haloalkanes are formed from open-chain hydrocarbons (alkanes), whereas haloarenes are derived from aromatic hydrocarbons.
    9 min read
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