interstitial
Oxygen that is dissolved in the water crossed ghe gill menbrane by diffusion. The oxygen is dissolved in the water like carbon dioxide in a beer. This oxygen is not a part of the water molecule. The oxygen in the water molecule is not available to the fish, when dosolved oxygen gets low, yhou have a fish kill.
Infinitely many. Infinitely many. Infinitely many. Infinitely many.
Infinitely many. Infinitely many. Infinitely many. Infinitely many.
so many hours
The type of lamellae found between osteons is interstitial lamellae. These lamellae are remnants of old osteons that have been partially destroyed during bone remodeling.
The layers of calcified matrix in bone tissue are called lamellae. These lamellae are arranged in concentric circles around central canals called Haversian canals, forming the structure known as an osteon or Haversian system.
The membranes connecting the grana in chloroplasts are called stroma lamellae. They connect the thylakoid stacks (grana) and play a role in facilitating communication and transport of molecules within the chloroplast.
The matrix rings are called lamellae and they concentrically surround the central canal (Haversian canal) of each osteon. They form a series of concentric circles, providing structural support and strength to the bone tissue.
Concrete lamellae
Concentric lamellae.
Fish have lamellae in their gills. As the water flows through the gills and over the lamellae, the oxygen is extracted from the water.
The hyphae terminate in radiating lamellae in the gills of a mushroom. These gills are found underneath the cap and are responsible for producing and dispersing spores.
It circulation
interstitial
yes it is in spongy and bone
Exsolution lamellae are formed when a high-temperature, high-pressure mineral undergoes cooling and decompression. During this process, the mineral separates into two distinct compositions, leading to the formation of lamellae within the crystal structure. This phenomenon occurs due to changes in the solubility of different mineral components as the conditions for the mineral's formation change.