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関連する概念動画

The Structure of Intermediate Filaments01:19

The Structure of Intermediate Filaments

The intermediate filaments are one of three widely studied cytoskeletal filaments. They are so named as their diameter (10 nm) is in between that of microfilaments (7 nm) and the microtubules (25 nm).  These filaments are highly stable and can remain intact when exposed to high salt concentrations and detergents. These filaments are responsible for providing stability and mechanical support to the cells. They also help in cell adhesion and maintaining tissue integrity.
Intermediate filaments...
Structures of Solids02:22

Structures of Solids

Solids in which the atoms, ions, or molecules are arranged in a definite repeating pattern are known as crystalline solids. Metals and ionic compounds typically form ordered, crystalline solids. A crystalline solid has a precise melting temperature because each atom or molecule of the same type is held in place with the same forces or energy. Amorphous solids or non-crystalline solids (or, sometimes, glasses) which lack an ordered internal structure and are randomly arranged. Substances that...
Transition Zone01:28

Transition Zone

The transition zone in concrete is a critical area where aggregate meets cement paste, marked by a distinct porosity and weakness compared to the surrounding material. The adhesion around the aggregates is primarily due to Van Der Waals forces. The voids within this zone influence its robustness; initially, it is less durable than the surrounding bulk mortar due to larger voids. Initially, when concrete is compacted, a higher water-cement ratio near the aggregates leads to the formation of...
Intermolecular Forces03:13

Intermolecular Forces

Atoms and molecules interact through bonds (or forces): intramolecular and intermolecular. The forces are electrostatic as they arise from interactions (attractive or repulsive) between charged species (permanent, partial, or temporary charges) and exist with varying strengths between ions, polar, nonpolar, and neutral molecules. The different types of intermolecular forces are ion–dipole, dipole–dipole, hydrogen bonds, and dispersion; among these, dipole–dipole, hydrogen bonds, and dispersion...
Bricks01:14

Bricks

Bricks, a fundamental building material, are crafted from fired clay and exhibit a range of shapes, sizes, and colors. The production process starts with extracting local clay or shale, which is then crushed, ground, and screened for a fine texture. The refined material is blended with water, creating a pliable mixture that can be formed into bricks using one of three processes: soft mud, dry press, or stiff mud methods.
Soft mud bricks are shaped in molds with high moisture content and can be...
Formation of Intermediate Filaments00:57

Formation of Intermediate Filaments

Intermediate filaments are cytoskeletal proteins with higher tensile strength and flexibility than microfilaments and microtubules. Unlike the other two cytoskeletal proteins, intermediate filament formation lacks the enzymatic activity to hydrolyze nucleotides like ATP and GTP to generate energy for polymerization. Therefore, the formation of intermediate filaments is multistep self-assembly. The involvement of any accessory proteins in intermediate filament formation has not yet been reported.

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関連する実験動画

Updated: Jul 12, 2026

Combined Size and Density Fractionation of Soils for Investigations of Organo-Mineral Interactions
08:38

Combined Size and Density Fractionation of Soils for Investigations of Organo-Mineral Interactions

Published on: February 15, 2019

基本粒子としての層間粘土.

P H Nadeau, M J Wilson, W J McHardy

    Science (New York, N.Y.)
    |August 31, 1984
    PubMed
    まとめ

    共通の層間粘土鉱物は,基本的な粒子の集合体である. 新しいモデルは,たったの3種類の粒子を用いて,粒子間 difraktionを通して,それらのX線 difraktion パターンを説明します.

    科学分野:

    • ミネラロジーは,鉱物学です.
    • マテリアルサイエンス 材料科学
    • 地質化学 地質化学

    背景:

    • 層間粘土鉱物は,多様な構造を持つ複雑な材料です.
    • 基本的な組成を理解することは,地質学や材料科学の応用において極めて重要です.

    研究 の 目的:

    • 層間粘土鉱物の新しいモデルを提案する.
    • 基本的な粒子の集積に基づいて,それらのX線 difraktion特性を説明するために.

    主な方法:

    • 送電電子顕微鏡 (TEM) を用いて粒子の構造を分析した.
    • X線 difraktion (XRD) は, difraktion パターンを研究するために使用されました.
    • 実験モデリングは,限られた基本的な粒子タイプを使用した.

    主要な成果:

    • 層間粘土鉱物は,基本的な粒子の集積から構成されています.
    • 3つの基本的な粒子タイプのみを使用して,幅広い層間構造パターンをモデル化することができます.
    • X線屈折パターンは,これらの集積物内の粒子間屈折から生じます.

    結論:

    さらに関連する動画

    Determination of the Settling Rate of Clay/Cyanobacterial Floccules
    06:00

    Determination of the Settling Rate of Clay/Cyanobacterial Floccules

    Published on: June 11, 2018

    Utilizing Soil Density Fractionation to Separate Distinct Soil Carbon Pools
    09:19

    Utilizing Soil Density Fractionation to Separate Distinct Soil Carbon Pools

    Published on: December 16, 2022

    関連する実験動画

    Last Updated: Jul 12, 2026

    Combined Size and Density Fractionation of Soils for Investigations of Organo-Mineral Interactions
    08:38

    Combined Size and Density Fractionation of Soils for Investigations of Organo-Mineral Interactions

    Published on: February 15, 2019

    Determination of the Settling Rate of Clay/Cyanobacterial Floccules
    06:00

    Determination of the Settling Rate of Clay/Cyanobacterial Floccules

    Published on: June 11, 2018

    Utilizing Soil Density Fractionation to Separate Distinct Soil Carbon Pools
    09:19

    Utilizing Soil Density Fractionation to Separate Distinct Soil Carbon Pools

    Published on: December 16, 2022

    • 新しいモデルは,層間粘土鉱物を基本的な粒子の集団として見ています.
    • このモデルは,観測されたX線 difraktionの特徴をうまく説明しています.
    • この発見は,複雑な粘土鉱物構造の理解を簡素化する.