Nutrition, University of California,
INTRODUCTION In view of the recent comprehensive reviews by Robertson (13) and by Hewitt (4) and because of the fact that detailed annual coverage of the subject is readily available in abstract form, it was felt desirable to confine this article largely to the basic feature of mineral nutrition, namely, Mechanism of Ion absorption by roots.
Passive Absorption of water
This Mechanism of Ion Absorption is performed without the use of metabolic energy. Here, the root works only as absorption or passive device. Therefore, it is sometimes referred to as “water absorption through the root” rather than “water absorption through the root”. Due to the opening of stomata and weather conditions, it occurs in plants that multiply rapidly during the day. The force to absorb water is generated at the end of the leaf, which is the transpiration effect. The main reason behind transpiration is to raise water along the axis of the plant, just as a person raises a bucket of water from the well. The transpiration withdrawal is responsible for drawing water at the end of the leaf, and the pull or force is transferred to the root via the water column in the wood texture component. Due to the strong cohesion between the particles, the continuity of the water column remains unchanged, and it acts as a rope.
The root simply acts as a passive absorption device. As transpiration advances, water absorption occurs simultaneously to compensate for water loss at the tip of the blade. Most of the water entering the plant is achieved through passive absorption. Negative transfer is not different from diffusion, it does not require energy input: the molecules move freely from higher concentrations to lower ones. Water will enter the plant through the root cells, which can be found in the roots where passive absorption occurs mainly. In addition, when absorbing water, minerals, and nutrients are also absorbed.
Active Absorption of water
Active absorption means that the roots produced by the respiration of the root absorb water with the help of adenosine triphosphate: where the root cells are actively involved in this process, they are called active absorption. According to Renner, active absorption occurs in plants with low transpiration and sufficient water, where 4% of the total water absorption is performed. Active absorption is carried out through two theories: active permeable water and active impermeable active water. In the process, no power is required.
Difference between Active and Passive Water Absorption
|Sl. No.||Active Absorption||Passive Absorption|
|1||Active absorption of water utilizes metabolic energy||Passive absorption utilizes solar energy|
|2||Water is absorbed ‘by’ the roots (Roots have an active role)||Water is absorbed ‘through’ the roots (Roots have only a passive role)|
|3||The water is absorbed by osmosis and non-osmosis method along or against the DPD gradient||Water is absorbed as a result of the tension created by the transpiration pull|
|4||Involves symplast * (protoplast) movement of water||It involves apoplast * (nonliving part) movement through free spaces|
|5||Absorption is independent of transpiration||Absorption is dependent on transpiration|
|6||Usually, takes place when the water level is high in the soil||Usually, takes place when the water level is low in the soil|
|7||Occur only in the presence of roots||Occurs even in the absence of roots|
|8||Produce positive pressure in the xylem canals||Produce negative pressure in the xylem canals|
|9||The absorption rate is comparatively slow||The absorption rate is comparatively fast|
|10||Quickly inhibited by metabolic inhibitors or toxins||Metabolic inhibitors or toxins do not have an immediate effect on passive absorption|
|11||Two types: (1) Active osmotic water absorption and (2) Active non-osmotic water absorption||No such classification in passive water absorption|
Understandably, over the past 30 years, there has been a growing interest in the process of mineral absorption by plant cells. From the point of view of practical agriculture, the absorption reactions are intimately tied up with nutritional and toxicity problems in connection with the growing of crops in soil. Also, since the process frequently involves the accumulation of elements in cells against gradients in chemical potential, the phenomenon of ion absorption is of considerable theoretical interest. Just as photosynthesis in plants has aroused the curiosity of physiologists and chemists in that it represents a transformation of radiant energy into chemical energy, so also is ion absorption of interest because apparently it involves a transformation of chemical energy into osmotic energy.
As the study of mineraluptake by plant and animal cells has progressed over recent decades, theoriesand mechanisms designed to explain the process have been proposed in abundance.These mechanisms fall roughly into two general classes; namely, (a) those whichinterpret the process in terms of special physical or electricalcharacteristics of cellular membranes, and (b) those which postulate regionswith special chemical properties. In general, it can be said that the averagelife of these theories has been short because of the continual uncovering ofnew experimental evidence which has placed fresh burdens on or completelyeliminated existing theories.
As matters stand atpresent, no proposed mechanism for ion absorption is universally accepted.Nevertheless, the salient features of the process have been reasonably wellestablished for a variety of plant tissues. Thus we are at least in a favorableposition to weigh and evaluate theories as they are proposed. Morespecifically, any theory of ion uptake by roots must be consistent with thefollowing uniformly observed facts concerning the process:
The ion adsorption process requires metabolic activity by the plant (isotopic exchanges excepted). Onion accumulation occurs in the absence of respiration and other activities such as protein synthesis, etc. In general, the process is an attribute of tissues capable of growth although not invar.
You Might Also Like: