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Published edits to the article on "Hydraulic Redistribution".


Adding to a pervious article on “Hydraulic Redistribution” on Wikipedia

Will be adding mycorrhizal associations to an article that already talks about vascular plants

Hydraulic Redistribution[edit]

Hydraulic redistribution is a passive mechanism where water is transported from dry to water soils by subterranean networks[1]. This occurs in vascular plants that commonly have roots in both wet soil and extremely dry soil, especially plants with both taproots that grow vertically down to the water table, and lateral roots that sit close to the surface.


Process[edit]

Hot, dry periods, when the surface soil dries out to the extent that the lateral roots exude whatever water they contain, will result in the death of such lateral roots unless the water is replaced. Similarly, under extreme wet conditions when lateral roots are inundated by flood waters, oxygen deprivation will also lead to root peril. In plants that exhibit hydraulic redistribution, there are xylem pathways from the taproots to the laterals, such that the absence or abundance of water at the laterals creates a pressure potential analogous to that of transpirational pull. In drought conditions, ground water is drawn up through the taproot to the laterals and exuded into the surface soil, replenishing that which was lost. Under flooding conditions, plant roots perform a similar function in the opposite direction. For a visualization of this process, see "Hydraulic Redistribution Cartoon," Dawson Lab, UC Berkeley, CA.

Though often referred to as hydraulic lift, movement of water by the plant roots has been shown to occur in any direction.[1][2][3] This phenomenon has been documented in over sixty plant species spanning a variety of plant types (from herb and grasses to shrubs and trees)[4][5][6] and over a range of environmental conditions (from the Kalahari Desert to the Amazon Rainforest).[4][5][7][8]

Causes[edit]

The movement of water can be explained by the cohesion-tension theory throughout a plant. In brief, it states that movement of water through the plant depends on having a continuous column of water, from the roots to the leaves. Water is then pulled from the roots to the leaves, through the plant system, by the difference in water potential between the boundary layers of the soil and the atmosphere. Therefore, the driving force for moving water through a plant is the cohesive strength of water molecules and a pressure gradient from the roots to the leaves. This theory can still be applied when the boundary layer to the atmosphere is closed, e.g. when plant stomata are closed or in senesced plants. [9] The pressure gradient is between soil layers with different water potentials; water moves through the roots from wetter to drier soil layers in the same manner as it does when the plant is transpiring.

Assisting Hydraulic redistribution[edit]

It has been understood that hydraulic lift aid in the host plant in the absorption of water and other vital nutrients [2]. At the time, “lift” described the movement of water and soil nutrients up the vascularized host which occurs mostly at night [2].

As defined by the instruments of time, hydraulic lift occurred at night due to the lower rates of transpiration in the host [2]. This allows the fungus to “redistribute” water to drier soils where water uptake was significant during the day [2].

Yet, in modern phasing, there consensus of using hydraulic redistribution as opposed to hydraulic lift [2]. This more comprehensive choice of words takes into consideration, the bi-directional and passive movement exhibited by the plant root that is facilitated by mycorrhizae [2][3].

Identifying mycorrhizal networks that could facilitate hydraulic redistribution

Ectomycorrhizae fungus

Arbuscular mycorrhizal fungus

There is a movement to understand the full extent of these mycorrhizae network starting in the late 1980s continuing on to today [2].

Today, there is a consensus that mycorrhizae networks can aid in seedling growth [3][4].

With finer instrumentation, there are more discoveries regarding new interactions between other mycorrhizae and their corresponding host. Even noticing interactions between other mycorrhizae to form a network that could support an ecosystem.

These studies usually focused on seedling growth and their intimate interactions between the fungal network.

Significance[edit]

The ecological importance of hydraulically redistributed water is becoming better understood as this phenomenon is more carefully examined. Water redistribution by plant roots has been found influencing crop irrigation, where watering schemes leave a harsh heterogeneity in soil moisture. The plant roots have been shown to smooth or homogenize the soil moisture. This sort of smoothing out of soil moisture is important in maintaining plant root health. The redistribution of water from deep moist layers to shallow drier layers by large trees has shown to increase the moisture available in the daytime to meet the transpiration demand.

The implications of hydraulic redistribution seem to have an important influence on plant ecosystems. Whether or not plants redistribute water through the soil layers can affect plant population dynamics, such as the facilitation of neighboring species. [10] The increase in available daytime soil moisture can also offset low transpiration rates due to drought (see also drought rhizogenesis) or alleviate competition for water between competing plant species. Water redistributed to the near surface layers may also influence plant nutrient availability. [11]

Observations and modeling[edit]

Due to the ecological significance of hydraulically redistributed water, there is an ongoing effort to continue the categorization of plants exhibiting this behavior and adapting this physiological process into land-surface models to improve model predictions.

Traditional methods of observing hydraulic redistribution include Deuterium isotope traces,[3][5][8][12] sap flow,[4][7][13][14] and soil moisture.[2][5] In attempts to characterize the magnitude of the water redistributed, numerous models (both empirically and theoretically based) have been developed.[15]

References:[edit]

  1. ^ Allen, Michael F.; Vargas, Rodrigo; Prieto, Iván; Egerton-Warburton, Louise M.; Querejeta, José Ignacio (2012-06-01). "Changes in soil hyphal abundance and viability can alter the patterns of hydraulic redistribution by plant roots". Plant and Soil. 355 (1–2): 63–73. doi:10.1007/s11104-011-1080-8. ISSN 1573-5036.
  2. ^ a b c d e f g "Water transport in trees: current perspectives, new insights and some controversies". Environmental and Experimental Botany. 45 (3): 239–262. 2001-06-01. doi:10.1016/S0098-8472(01)00074-0. ISSN 0098-8472.
  3. ^ a b Querejeta, José I.; Navarro-Cano, José A.; Alguacil, María del Mar; Huygens, Dries; Roldán, Antonio; Prieto, Iván (2016-09-01). "Species-specific roles of ectomycorrhizal fungi in facilitating interplant transfer of hydraulically redistributed water between Pinus halepensis saplings and seedlings". Plant and Soil. 406 (1–2): 15–27. doi:10.1007/s11104-016-2860-y. ISSN 1573-5036.
  4. ^ Simard, Suzanne; Bingham, Marcus A. (2012-03-01). "Ectomycorrhizal Networks of Pseudotsuga menziesii var. glauca Trees Facilitate Establishment of Conspecific Seedlings Under Drought". Ecosystems. 15 (2): 188–199. doi:10.1007/s10021-011-9502-2. ISSN 1435-0629.