Showing posts with label Below-Ground Services. Show all posts
Showing posts with label Below-Ground Services. Show all posts

Wednesday, October 13, 2021

Trees in the vineyard (Agroforestry) and the effect on grapevine root systems

Agroforestry is one of the key soil health and land management practices of the Regenerative Organic Certification. The practice, as defined by the US Department of Agriculture (USDA), involves "the intentional integration of trees and shrubs into crop and animal farming." Trees provide a number of below- and above-ground services which may be of benefit to the viticulturist (documented by Favor). I have previously reported on the impact of trees on vineyard water parameters and soil-based nutrients. I continue herein with an examination of the effect of trees on vine root systems. Portions of this post draws heavily on the research reported out in Favor's work.

Soil Structure
The vineyard site is a key variable in the production of high-quality grapes, which is, itself, a key requirement for the production of high-quality wine. According to Wolf and Boyer (Vineyard Site Selection, Virginia Cooperative Extension), the best vineyard soils "permit deep and spreading root growth" and provide a moderate supply of water year-round. Katherine Favor posits that "much of the ability of vines to absorb both water and nutrients in the face of competition depends on the health and spatial distribution of the vine's root system" with research suggesting that "the depth and expansion of grapevine roots is highly dependent on soil structure and permeability ... and that grapevine root plasticity is also influenced by planting density and competition." 

What are the soil characteristics that will permit "deep and spreading root growth" and year-round access to water?  The most important requirements are internal water drainage and water-holding capacity. Geologic permeability (the capability of a porous rock or sediment to permit the flow of fluids through its pore spaces -- Dictionary.com) is seen by Wolf and Boyer as perhaps the most important consideration in a candidate vineyard's soil. Mark Chien (Soil and Site Selection Considerations for Wine Grape Vineyards, Pennsylvania State University) sees well-drained soils as a common denominator among all great vineyard sites. These soils "strike a balance between adequate depth and drainage and water-holding capacity" and vines deployed therein will have adequate water access during the summer and can rapidly drain water from the soils in the event of rainfall during the grape-ripening period. According to Favor, soil porosity is an even more important determinant of grape quality than is nutrient availability.

Another key soil feature is effective rooting depth. According to UCDavis, about 60% of the root structure of a vine plant can be found in the first two feet of the surface but individual roots can grow as deep as 20 feet, depending on soil permeability, the level of the water table, and the rootstock variety.

According to Favor, the above characteristics, among others, are influenced by soil structure. Soil structure -- the spatial arrangement of individual soil particles, their aggregates, and the pore space between them -- "affects soil strength, water holding capacity, nutrient retention, aeration, friability, erodibility, plant root movement and biological activity." A high-quality soil structure allows for deeper and stronger vine root systems and higher grape production quality. Soil quality characteristics are summarized in the chart below.


Agroforestry's Impact on Soil Structure
Agroforestry has been shown to improve soil structure through a variety of mechanisms (Favor):
  • A mulching effect from litterfall and pruning materials can have beneficial effects on topsoil structure
    • Soil cover improves soil structure by reducing raindrop and irrigation effect → conserved surface macroporosity → greater water infiltration rates → improved soil penetration
  • High amounts of root biomass produced by the trees
    • Tree roots improve soil macroporosity by breaking up compacted soils and leaving behind old root channels that grapevine roots are able to occupy for greater rooting depth capability
    • Finer roots contribute to improved soil structure
    • Tree buffer treatments produced higher porosity, increased mesoporosity, and improved soil structure
  • Increased organic matter (OM) content
    • Soil structure is largely influenced by the amount of OM in the soil
    • Higher levels of OM → higher aggregate stability and overall improved structure
    • Higher levels of OM contribute to increasing water infiltration and fertility
    • Organic matter is able to use "sticky substances" to glue soil particles together → stable soil pores.
In summary, the agroforestry-related increase in OM → increased soil structure → increased rooting capability → higher yields and higher quality fruit production (Favor).

Competition Between Tree and Grapevine Roots
According to Favor, "much of the ability of vines to absorb both water and nutrients in the face of competition depends on the health and spatial distribution of the vines' root system." 

Research has shown an overlap in the activity spheres of plants and vines: 63% of grapevine roots are in the upper 60 cm of soil compared to 77% of conifer roots while 80% of grapevine roots are in the upper 1 m of soil compared to 91% for trees. Grapevines might have a deeper concentration of roots at deeper soil profiles as their remaining roots extend to depths of as much as 12 m. Grapevine roots can spread out up to 10 m laterally from the trunk.

The most frequent agroforesty applications to date are olive trees with grapevines. Olive trees have similar lateral-root experiences as does the grapevine but its vertical roots grow even deeper. Similar to the grapevine, olive trees absorb the majority of nutrients in the top 1 m of soil and water in the top 1.2 - 1.7 m of soil. As Favor concludes, there may be substantial below-ground overlap between these systems.

Competition notwithstanding, Favor concludes that:
The positive effects that trees impart on soil structure, soil quality and root plasticity allow for deeper and stronger root systems that can better absorb nutrients and water despite competition from trees ... Fracture lines left behind by tree roots allow opportunities for grapevines to grow even deeper than they otherwise would have ... Additionally, competition from tree roots can trigger grapevine root plasticity, which results in increased root length density and increased nutrient and water absorption capacity per cm of soil. Tree roots and grapevine roots are indeed able to adapt to competition and thrive despite occupying overlapping niches.
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This concludes our examination of the below-ground services provided by trees in an agroforestry system. As per Favor, "there is growing evidence that incorporating trees into vineyards could play a valuable role in the future of viticulture in the coming years."

I will next turn to examination of the above-ground services provided by trees in an agroforestry system.


©Wine -- Mise en abyme

Sunday, October 3, 2021

Trees in the vineyard (Agroforestry) and the impact on soil-based nutrients

Agroforestry, as it relates to viticulture, is concerned with the co-location of trees and vineyards. Trees provide a number of below- and above-ground services which may be of benefit to the viticulturist (documented by Favor). I have previously reported on the impact of trees on vineyard water parameters and continue herein with the effects on soil-based nutrients. The effects portion of this post draws heavily on the Favor work.

Background on Soil-based Nutrients
Adequate amounts of the appropriate nutrients are required to support proper growth of the grape vine, fruit development, and fruit maturity; those nutrients are obtained from the soil by the plant.  The table below shows the mineral requirements of the vine plant, the role of each mineral, acceptable ranges of each mineral in the soil, and the impact of mineral deficiency on the vine.

Source: Compiled from LGRGP.org and others

Sources
Rocks
The earth is made up of varying proportions of the 90 or so naturally occurring elements but, according to Alex Maltman (Vineyards, Rocks, & Soils), four of these -- oxygen at 48%, silicon at 28%, aluminum at 8%, and iron at 6% -- are responsible for 88% of its composition. In most geological materials, these elements combine to form minerals -- "a naturally occurring combination of specific elements that are arranged in a particular repeating three-dimensional structure or lattice" (opentextbc.ca, Minerals and Rocks).

In nature, minerals are found in rocks "and the vast majority of rocks are composed of at least a few different minerals." Jackson (Wine Science: Principles and Applications) stipulates that (p. 245) "... the mineral content of soil is primarily derived from the parental rock substrate." The figures below show the weathering of rocks into minerals.

Decaying Organic Material
Jamie Goode (Rescuing Minerality) contends that the bulk of soil mineral content comes "from decaying organic material, not decomposed rock and it is microbial activity in the soil that affects the ability of soil to break down organic matter into mineral ions that can be used by the plant." Maltman agrees with Goode: "... in practice, it's the humus that's more important, indeed essential."

Atmosphere
According to Schwarcz and Schoeninger (Stable Isotope Analysis in Human Nutrition, Yearbook of Physical Anthropology 34, pp. 293-321), almost 100% of exchangeable nitrogen is found in the atmosphere or dissolved in the world's oceans and is transferred from these environments into the biological system through the terrestrial nitrogen cycle.

Cation Exchange
Soil-based nutrients are resident either in the soil solution (water and dissolved minerals in the soil pores) or in the soil matrix (mineral particles and organic matter).  Two problems present themselves, however: (i) the concentration of nutrients in the soil solution is low and (ii) the nutrients resident in the soil matrix are immobile.  Plant roots have developed adaptions to allow growth into the soil matrix and capture of the nutrients needed for metabolic activity (Dr. Paul Schreiner, USDA-ARS) and we will discuss these later.

Most of the mineral nutrients that the vine needs are cations so the soil's cation exchange capacity (CEC) is a major enabler of  it's nutrient acquisition. The positively charged mineral ions bind loosely to the clay and humus colloids in the soil and these minerals are released in exchange for hydrogen ions secreted by the vine roots. (Clay minerals act as harbors for nutrients because the positive ions of the nutrients are trapped by the negative charge of the clay minerals.  The abundance and types of minerals determine whether the clay is classed as low- or high-CEC.). The ion that makes the strongest link with the clay is the hydrogen ion "... and its almost as though the vine knows this! The vine's metabolism can prompt its roots to pump out hydrogen ions into the soil water, which then dislodges the other ions held on the clays, thus making them available to the vine roots" (Maltman). 

The Effect of Trees on Vine Nutrition Parameters
The effect of trees on vine nutrition parameters are summarized in the chart below and described in greater detail in the sections following.


Increased Nutrient Availability
As shown in the chart above, trees increase nutrient availability by increasing organic matter, cycling nutrients from deep to shallow profiles, fixing nitrogen, and transforming nutrients into a more plant-absorbable form.  

As regards organic matter (Favor):
  • Agroforestry systems have the potential to increase this material by 50 to 100% 
    • They return an average of 7.4 tons of organic matter/ha/year in the form of prunings
      • They also produce organic matter through litterfall, root slough, and root exudates
    • Nutrients that take the form of organic matter are released slowly at rates comparable to rates of plant absorption 
      • They also present in a stable molecular form that is resistant to leaching
    • Organic matter produced by trees serves as a source of food for microbes
      • Results in increased microbial populations (by as much as 30%)
      • Microbes excrete enzymes that mineralize nutrients, stabilize carbon and N in the soil, and decompose organic matter into simple, plant-available forms
        • Results in higher plant nutrient uptake
    • Results in increased cation exchange capacity
      • Translates to a greater ability of soil to hold onto exchangeable cations
      • Better retention of applied nutrients
      • Resistance from nutrient leaching
  • Nutrients that take the form of organic matter are released slowly at rates comparable to rates of plant absorption
    Trees cycle nutrients from deeper profiles by accessing those nutrients deep underground, converting them into plant tissue and organic material, and dropping organic material to the ground in the form of leaf-litter and above-ground debris. As this material degrades, it releases nutrients into the upper soil profiles where they become available for use by other crops (Favor).

    Almost 100% of exchangeable nitrogen is found in the atmosphere or dissolved in the world's oceans and is transferred from these environments into the biological system through the terrestrial nitrogen cycle illustrated in the figure below.  

    Source: http://tolweb.org/notes/?note_id=3920

    Depending on the species, trees can fix nitrogen at average rates of 40 to 200 kg N/ha/yr (Favor).

    Finally, the increased microbial life -- resulting from the tree-related increase in organic material -- excrete enzymes that decompose organic material into simple, plant-available forms, resulting in higher plant nutrient uptake.

    Reduced Nutrient Loss
    By reducing nutrient losses from leaching, erosion, and runoff, trees allow the retention of  greater amounts of soil-based nutrients in the vineyard. According to Favor:
    • Agroforestry systems increase soil organic by as much as 100% with as little as a 10% increase decreasing soil erodibility by between 13 and 23%
    • Litterfall increases ground cover which reduces runoff and erosion
    • Surface mulch associated with agroforestry systems reduces the kinetic impact of rainfall, retaining the soil surface structure.
    Competition Between Trees and Grapevines
    At distances of less than 4 m, there is intense competition for nutrients, especially nitrogen, between plants and grapevines. The negative effects observed were reduced vine vigor and yield with no obvious effect on berry quality. Beyond 4 m, no negative competitive effects were observed.


    ©Wine -- Mise en abyme