Radium primarily produces a steady stream of alpha particles as it undergoes radioactive decay. These alpha particles are helium nuclei, consisting of two protons and two neutrons, and are emitted during the decay process of radium isotopes. This emission is a characteristic feature of radium's radioactivity and contributes to its use in various applications, including radiotherapy.
The answer is carrying capacity.
Medication in your blood stream is flushed out through your kidneys or by your liver into your digestive tract. Your kidneys usually do not remove large compounds from your blood stream, but small ones. By having the active particle in the medicine larger than the particles the kidneys remove from the blood stream, the kidneys will not flush out the medicine. Sometimes this is done by pegylating the medicine particle. That simply adds a propylene glycol particle to the medicine particle. When the medicine gets to where it is needed, the peg drops off. Eventually the pegs drop off and the medicine is either used or eliminated.
If your cells can't get a steady stream of glucose, the cell will die.
If your cells can't get a steady stream of glucose, the cell will die.
The maximum size particle a stream can carry is primarily controlled by the stream's velocity and discharge, which is the volume of water flowing per unit of time. Faster-moving water can transport larger and heavier particles due to increased kinetic energy. Additionally, the stream's gradient and channel shape can influence sediment transport, with steeper gradients typically facilitating the movement of larger particles. Lastly, the sediment's shape and density also play a role in determining its transport capacity.
The largest size particle that a stream can carry is typically referred to as the stream's competency limit. This limit is reached when the stream's velocity is no longer able to transport a particle of a certain size due to its weight and shape, causing the particle to be deposited on the streambed instead.
electric current
Stream Scheduling is a scheduling system where there is a steady stream/flow of patients at set appointments throughout the day.
When stream flow decreases to below the critical settling velocity of a certain size particle, the particle will settle out of suspension and deposit on the streambed. This process is known as sediment deposition and is influenced by factors such as stream velocity, particle size, and sediment concentration.
Electric charge flowing in a steady stream is called electric current. It is the rate of flow of electric charge and is measured in Amperes (A).
If there is not a steady stream of cool air blowing over the motor and heating coil and removing heat from them, they will instantly burn out. (Been there. Done that.)
The minimum stream velocity needed to carry a particle of sand depends on the size and weight of the sand particle, as well as the characteristics of the stream such as flow rate and turbulence. In general, for typical sand particles, a stream velocity of around 0.3 m/s to 1 m/s is needed to entrain and transport them.
The answer is carrying capacity.
The measure of the largest particles a stream can carry is capacity.
When stream flow decreases below the critical settling velocity of a certain size particle, the particle will settle out of the flow and deposit on the streambed. This process is known as sedimentation and can lead to the formation of sediment layers along the stream channel. Over time, these deposits can alter the shape and depth of the stream channel.
Transport hydrophobic substances in the blood stream.
The minimum stream velocity needed to keep a particle in motion can be estimated using the settling velocity equation. For a 10 cm diameter particle, the approximate minimum stream velocity would need to be around 0.03 m/s to keep it in motion. This value may vary depending on factors such as particle density and fluid properties.