Soil Region's Really Matter

Mark Webber • Mar 25, 2018

What Soil and Soil Regions of O,A,B and C are you trying to grow your plants in?

One of the classic comments that property owners like to say is: " my soil is lousy" . However, to determine how great or mediocre your soil is you need to conduct the proper investigation of the conditions in any site to decide what plants will or will not grow. Unfortunately without the adequate investigation of soil conditions the choices made in plant selection and fertility treatments may not adequately meet the conditions that actually exist.

The National Cooperative Soil Survey identifies and maps over 20,000 different kinds of soil in the United States. Most soils are given a name, which generally comes from the locale where the soil was first mapped. Named soils are referred to as soil series. Soil survey reports include the soil survey maps and the names and descriptions of the soils in a report area. These soil survey reports are published by the National Cooperative Soil Survey and are available to everyone.

Soils are named and classified by physical and chemical properties in their horizons (layers). “Soil Taxonomy” uses color, texture, structure, and other features of the surface two meters deep to key the soil into a classification system to help people use soil information. This system also provides a common language for scientists and people making choices about plant selection and management.

Soils and their horizons differ from one another, depending on how and when they formed. Soil scientists use five soil factors to explain how soils form and to help them predict where different soils may occur. The scientists also allow for additions and removal of soil material and for activities and changes within the soil that continue each day. Soil Forming

Factors that create soils

Parent material
Few soils weather directly from the underlying rocks. These “residual” soils have the same general chemistry as the original rocks. More commonly, soils form in materials that have moved in from elsewhere. Materials may have moved many miles or only a few feet. Windblown “loess” is common in the Midwest. It buries “glacial till” in many areas. Glacial till is material ground up and moved by a glacier. The material in which soils form is called “parent material.” In the lower part of the soils, these materials may be relatively unchanged from when they were deposited by moving water, ice, or wind. Sediments along rivers have different textures, depending on whether the stream moves quickly or slowly. Fast-moving water leaves gravel, rocks, and sand. Slow-moving water and lakes leave fine-textured material (clay and silt) when sediments in the water settle out.

Climate
Soils vary, depending on the climate. Temperature and moisture amounts cause different patterns of weathering and leaching. Wind redistributes sand and other particles, especially in arid regions. The amount, intensity, timing, and kind of precipitation influence soil formation. Seasonal and daily changes in temperature affect moisture effectiveness, biological activity, rates of chemical reactions, and types of vegetation.

Topography
Slope and aspect affect the moisture and temperature of the soil. Steep slopes facing the sun are warmer, just like the south-facing side of a house. Steep soils may be eroded and lose their topsoil as they form. Thus, they may be thinner than the more nearly level soils that receive deposits from areas upslope. Deeper, darker colored soils may be expected on the bottom land.

Biological factors
Plants, animals, micro-organisms, and humans affect soil formation. Animals and micro-organisms mix soils and form burrows and pores. Plant roots open channels in the soils. Different types of roots have different effects on soils. Grass roots are “fibrous” near the soil surface and easily decompose, adding organic matter. Taproots open pathways through dense layers. Micro-organisms affect chemical exchanges between roots and soil. Humans can mix the soil so extensively that the soil material is again considered parent material. The native vegetation depends on climate, topography, and biological factors plus many soil factors such as soil density, depth, chemistry, temperature, and moisture. Leaves from plants fall to the surface and decompose on the soil. Organisms decompose these leaves and mix them with the upper part of the soil. Trees and shrubs have large roots that may grow to considerable depths.

Time
Time for all these factors to interact with the soil is also a factor. Over time, soils exhibit features that reflect the other forming factors. Soil formation processes are continuous. A recently deposited material, such as the deposition from a flood, presents no features from soil development activities. The previous soil surface and underlying horizons become buried. The time clock resets for these soils. Terraces above the active floodplain, while genetically similar to the floodplain, are older land surfaces and exhibit more development features.

These soil forming factors continue to affect soils even on “stable” landscapes. Materials are deposited on their surface, and materials are blown or washed away from the surface. Additions, removals, and alterations are slow or rapid, depending on climate, landscape position, and biological activity.

When mapping soils, a soil scientist looks for areas with similar soil-forming factors to find similar soils. The colors, texture, structure, and other properties are described. Soils with the same kind of properties are given taxonomic names. A common soil in the Midwest reflects the temperate, humid climate and native prairie vegetation with a thick, nearly black surface layer. This layer is high in organic matter from decomposing grass. It is called a “mollic epipedon. ” It is one of several types of surface horizons that we call “epipedons.” Soils in the desert commonly have an “ ochric” epipedon that is light colored and low in organic matter. Subsurface horizons also are used in soil classification. Many forested areas have a subsurface horizon with an accumulation of clay called an “argillic” horizon.

Soil Orders
Soil taxonomy at the highest hierarchical level identifies 12 soil orders. The names for the orders and taxonomic soil properties related to Greek, Latin, or other root words that reveal something about the soil. Sixty-four suborders are recognized at the next level of classification. There are about 300 great groups and more than 2,400 subgroups. Soils within a subgroup that have similar physical and chemical properties that affect their responses to management and manipulation are families.

Soil Horizons
Most naturally soil horizons have an "O,""A,""B" and a "C" horizons. The O horizon is at the very top and resulted from recent decomposition of organic matter. The A horizon is the fertile topsoil that in most cases of where plants derive nutrients and a lot of biological activities are occurring. The B horizons will have plant roots, and these are the areas of the soil that become critical to tree survival during excess drought conditions and anchorage. The C horizons are very limited in nutrient availability, have little to no organic matter and very low on oxygen. Many cases the soils that exist in the urban landscape today contain a large portion of C horizon soils that have mixes of A and B horizons. The A and B are buried under the C horizons. The C horizons can be made productive under proper management and treatments.

Soils In A Urban Reality

Many cases these original plotted conditions have changed due to urbanization. The horizons in many instances are inverted, and the rich plant regions of O, A, and B are buried by the C horizons. So its imperative that you anyone making decisions about fertility, plant selection, and plant management determine the chemical, physical and biological conditions of the soil in which you are managing in your landscape. The C horizons can be made productive under proper management and treatments.

Help is only a phone call away

Mark Webber's Landscaping conducts 1000' of soil tests for clients, and we advise plant owners and managers how to best manage your landscape, and what plants will or won't work in their landscaping.

https://www.webberlandscaping.com/testing-and-analysis

By Mark Webber 08 Mar, 2023
Often the public thinks that they can pick and place plants in their landscape like furniture. Before you plant anything do a investigation of the zone hardness, soils and other factors. It's always better to plan and investigate before you plant. Work with a qualified, certified and registered Arborist for the best results. https://www.webberlandscaping.com/landscape-designer
By Mark Webber 31 Aug, 2021
The fall armyworm (Spodoptera frugiperda) annually migrates northward, invading much of the continental United States and Canada. Many lawns in the month of August of 2021 are being eaten to death in the greater Dayton, Ohio area. The larval (caterpillar) stage of the fall armyworm moth can cause severe damage to lawns. In summer, the moths lay clusters of eggs in cotton-like, greenish-white masses on structures (houses, mailboxes, fences, signs, etc.), shrubs and trees, and the newly hatched larvae drop down to the ground and “march” like an army to feed on the closest grass. While the larvae are still small, damage may not be readily apparent. But when they reach their full size (about 1-1/2” long), they can eat the grass down to the soil. Significant infestations can defoliate a lawn entirely. Lush green grass is the fall armyworm’s preferred food, so irrigated lawns of any type (warm- or cool-season) are at most risk. So are newly laid sod and newly seeded or overseeded lawns since these must be kept moist/irrigated until the new grass establishes roots. Controlling fall armyworms is difficult since several generations can occur in one summer-through-fall season. Products that contain carbaryl (such as Sevin) or pyrethroids will be most effective while the larvae are still small. Mowing the turf and light irrigation before treatment can increase control. Repeat treatments may be necessary. Resources: https://turf.cals.cornell.edu/pests-and-weeds/insect-management/#caterpillars Potter, D.A. and S.K. Braman. 1991. Ecology and management of turfgrass insects. Annu. Rev. Entomol. 36:383–406.
By Mark Webber 24 Apr, 2021
By Mark Webber 13 Mar, 2021
Many homes are often constructed or renovated near existing trees to take advantage of their aesthetic and environmental value. Unfortunately, the processes involved with construction can be deadly to nearby trees. Recently we were assigned by a property owner to determine the health and condition of three trees commonly known as Silver Maple( Acer saccharinum). The property owner had recently purchased the property and had no information about the subject trees' prior treatment. The client was advised that we needed to conduct a starch test of each subject tree's condition. Starch tests provide the inspecting arborist a measure of the carbohydrate capacity of the tree in question. All green plants produce sugar (energy)in their leaves during photosynthesis. The sugar is then either used in the leaves as an energy source for the growth or production of other essential materials or transported via the phloem (inner bark) to other parts of the tree. The sugar that is not used immediately is linked together in long chains to create starch. Starch is the product the tree uses to store much of its energy reserves. By staining wood for starch, the level of the tree's energy reserves can be estimated. This information is beneficial when making a diagnosis of the tree's condition. Our testing of these three trees determined that they were collective in poor condition since the starch tested yielded light color wood. If a tree is in good condition related to carbohydrate reserves, then the starch test will yield a dark-colored wood when exposed to the iodine mixture. We discovered that these three trees had been severely injured ten years prior due to construction injury due to sidewalks, street curb, and underground pipe installation after reviewing our historical files and data. These subject trees have poor growth rates, limb loss, decay, and are becoming a hazard to the public and property. The necessary take-home lesson is that trees are often the victim of people pressure disease(PPD). With good arboricultural and horticultural advice, PPD can be avoided if the tree's owner is willing to follow a qualified arborist's advice and guidance when managing their trees. To learn how to manage trees that may be exposed to construction injury click here .
By Mark Webber 06 Mar, 2021
Learn how Mark Webber's Landscaping Company is saving Century-Old Oak's
By Mark A. Webber 29 Aug, 2020
By Mark Webber 01 Aug, 2020
In the growing season of 2020, I have witnessed an increasing frequency of trees being injured and damaged by the improper applications of pesticides targeting weeds in lawns. For the most part, these pesticides are herbicides that are commonly known as synthetic auxin. Synthetic auxin herbicides are used often on residential and commercial properties for broadleaf weed control. Trees and plants damaged by these pesticides often have these symptoms: Twisted leaves Downward cupping on leaves Narrow, strap-like leaves on the youngest growth Synthetic auxin herbicides are products commonly known as 2,4-D, Dicamba, Weed Be Gone, and others. These materials are manufactured to mimic naturally occurring plant hormones. There are five types of hormones in plants that include auxins. Plant hormones are triggering devices in plants. Plant hormones are triggering mechanisms that cause growth, leaf drop/formation, root expansion, flower bud formation, and other plant processes. In the case of herbicides that contain synthetic auxins, they mimic naturally occurring auxins that result in uncontrolled cell division. The uncontrolled cell division causes plants like broadleaf weeds and or trees certain death or severe damage. Many cases, the herbicides with synthetic auxins are indiscriminate broadleaf plant killers, especially if your tree has roots growing under your grassy lawn. Research has shown that trees have a massive root system that extends well beyond the tree's outer branches stretches over your yard. The root system of the trees in your lawn is made up of a vast network of the large, medium, and hair sized roots that are directly under the grass and weeds. Tree roots are not covered by bark, but are covered by the epidermis and have a multitude of root hairs. The roots of trees readily absorb water, nutrients, and pesticides. Roots of trees are not structured internally on a cellular level to filter out, so to speak harmful substances like herbicides containing synthetic auxins. So, even though you can't see any roots above your lawn from your trees, they are beneath your feet. The roots of your trees are just under the grass and the weeds. The roots of trees below the turf and weeds will readily absorb what's applied to the above-ground landscape. The majority of herbicides containing synthetic auxins forewarn users not to apply these products were tree roots exist. The label of these products is the legal requirements on how the product is to be used. The label of any pesticides is the law. If the applicator fails to follow the label, then that person is guilty of breaking the law. However, these label warnings are often ignored when the label states, "do not apply where tree roots exist." The failure to follow the labeling law results in damage, decline, and, in some cases, the death of trees. Herbicide injured trees can be killed and, in other cases, are more susceptible to diseases and insects and future decline. The bottom line is don't use herbicides that forewarn you not use them near trees and their root systems. If do you suspect that your trees have been exposed to herbicides, you should contact a qualified arborist for an inspection to investigate if your trees have been exposed to pesticides.
By Mark Webber 02 Mar, 2019
Photo Source (Tree Dictionary) This week I spent some time helping the team at Mark Webber's Landscaping conduct a tree risk assessment of a very large Ash tree. After the Ash inspection, I then inspected a number of other trees on the subject landscape. The property owner had unfortunately had her trees been mistreated by improper pruning. The term “seal,” rather than “heal,” is used to describe tree wound closure, since the wound still exists inside the tree even after it no longer shows on the outside. A properly pruned tree will create a better tree; however, a poorly pruned tree will result in a deteriorated condition. Trees have a natural defense response to wounds and pruning cuts. They form four types of walls to compartmentalize the area thus preventing the spread of decay organisms. However, if you prune too much from a tree, it will not have the energy resources to have the energy to compartmentalize. Proper pruning techniques and timing are critical to long-term tree health. The most important principle to remember is that each cut has the potential to change the tree considerably. Tree pruning needs to be well thought out and based upon what science and the Best Practices of the International Society of Arboriculture. In this case, the client's trees were excessively pruned by removing all of the subject inner branches resulting in a tree branch that looks like a lions tail. Lion's tail pruning creates tree branches that are likely to fail under normal weather conditions. In the case, the recommendation to this client was to do nothing or not to prune the subject trees for at least the next 6-9 years. Pruning Dose As a tree gets older the more difficult, it becomes for the plant to manage excess cuts. (See Chart/photograph above) When trees are young [Y] great amounts of symplast maintaining wood [L] can be removed. Symplastless wood is a term that is lucid to describe a tree or piece of wood or tree part that no longer maintains a symplast. As the tree matures [M] less symplast maintaining wood should be removed, and symplastless wood removal should increase [D]. As the tree approaches over maturity [OM] very little symplast maintaining wood [L] wood should be removed, and great amounts of symplastless wood [D] should be removed. Bottom Line If too many tree branches are removed or if the cuts are too large in older trees will result in further deterioration to the subject tree that may result in the loss of your valuable tree. You should use only Certified Arborist to make decisions about how to best manage your trees. Here are some important tips to follow for better trees: • Start training trees with pruning while they are young and newly established. • Minimize the number of live branches removed at any one time. • Use proper cuts. Watch the branch collar and/or branch bark ridge. • Pruning dose should be determined by overall tree health. • Reduce live-tissue pruning during times of drought. • Remove smaller branches rather than larger branches. • Do not top trees for any reason (heading cuts). • Prune when trees are biologically active to expedite wound sealing. • Do not use tree wound dressings. References http://www.treedictionary.com/DICT2003/tree_pruning/dose/chart.html Tree Pruning Essentials. Lindsey Purcell. Purdue University.2015 McKenzie, R. 2008. What’s Wrong with Topping Trees?, FNR-FAQ-14-W. Purdue University Cooperative Extension, West Lafayette, Ind., USA.
By Mark Webber 17 Feb, 2019
Trees are commonly injured. These injuries can cause structural defects if the tree does not successfully manage these damages by blocking water, bacteria and fungi.
By Mark Webber 03 Feb, 2019
Frost Cracks in trees and how to prevent and manage.
Show More
Share by: