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Horticulture Commons

Open Access. Powered by Scholars. Published by Universities.®

2010

Utah State University Extension

Articles 1 - 9 of 9

Full-Text Articles in Horticulture

Topsoil Quality Guidelines For Landscaping, Rich Koenig, Von Isaman Dec 2010

Topsoil Quality Guidelines For Landscaping, Rich Koenig, Von Isaman

Gardening

No abstract provided.


Solutions To Soil Problems: Ii. High Ph (Alkaline Soil), Loralie Cox, Rich Koenig Dec 2010

Solutions To Soil Problems: Ii. High Ph (Alkaline Soil), Loralie Cox, Rich Koenig

All Current Publications

PH is a measure of the acidity or alkalinity of a material. The pH scale ranges from 0 to 14, with 7 being neutral. A pH value below 7 indicates the soil is acidic, while values above 7 are alkaline. Each unit change in the pH scale is a 10-fold difference in acidity or alkalinity. For example, soil with a pH of 8 is ten times more alkaline than soil with a pH of 7.


Solutions To Soil Problems: I. High Salinity (Soluble Salts), Vernon Parent, Rich Koenig Dec 2010

Solutions To Soil Problems: I. High Salinity (Soluble Salts), Vernon Parent, Rich Koenig

All Current Publications

Salinity is a measure of the total amount of soluble salts in soil. As soluble salt levels increase, it becomes more difficult for plants to extract water from soil. Some plants are more resistant than other’s, but as the salt levels exceed their ability to extract water, they become water stressed.


Solutions To Soil Problems: Iv. Soil Structure, Rich Koenig, Teresa Cerny Dec 2010

Solutions To Soil Problems: Iv. Soil Structure, Rich Koenig, Teresa Cerny

All Current Publications

Soil structure refers to the combination of primary soil particles – sand, silt and clay – into larger units called aggregates or clods. Aggregates are commonly seen when a soil is tilled or disturbed.


Solutions To Soil Problems: V. Low Organic Matter, Kevin Heaton, Rich Koenig Dec 2010

Solutions To Soil Problems: V. Low Organic Matter, Kevin Heaton, Rich Koenig

All Current Publications

Utah soils are inherently low in organic matter due to the desert climate and historically low plant growth rates. In Utah, soil organic matter levels are typically 0.25 to 1%, while regions with high rainfall such as the Midwest and Eastern United States have soils with as much as 7 to 10% organic matter.


Turfgrass Cultural Practices And Insect Pest Management, Diane Alston, Kelly Kopp Sep 2010

Turfgrass Cultural Practices And Insect Pest Management, Diane Alston, Kelly Kopp

All Current Publications

There are a number of insects that can cause aesthetic and economic loss to turfgrass in Utah – in home lawns as well as in athletic fields and on recreational lands. Good turfgrass cultural practices are the primary way to prevent insect infestation and turfgrass damage.


Solutions To Soil Problems: Iii. Drainage, Michael Johnson, Rich Koenig Jun 2010

Solutions To Soil Problems: Iii. Drainage, Michael Johnson, Rich Koenig

All Current Publications

Drainage is a common problem throughout Utah. Complex patterns of soil development, transport and deposition have resulted in excessively drained soils that are coarse-textured (sandy or rocky), and poorly drained soils that are fine-textured (silt and clay-dominated). Excessively drained are more common in higher elevation and bench areas.


Cover Crops For Utah Gardens, Michael Johnson, Maggie Wolf, Rich Keonig Jun 2010

Cover Crops For Utah Gardens, Michael Johnson, Maggie Wolf, Rich Keonig

All Current Publications

No abstract provided.


Planting Landscape Trees, Michael R. Kuhns, Margaret Shao May 2010

Planting Landscape Trees, Michael R. Kuhns, Margaret Shao

All Current Publications

Trees and shrubs are valuable additions to most property, providing beauty, wind protection, shade, wildlife habitat, visual screening, and other benefi ts. Unfortunately, many landscape trees are not properly planted or cared-for.