- soil aggregate stability (up to 80%) – the ability of soil to resist erosion
- microbial biomass (up to 54%) – the mass of microscopic soil organisms driving nutrient cycling and carbon sequestration
- soil organic matter (up to 23%) – the living and dead carbon-containing part of the soil (central to healthy soils)
- maximum water-holding capacity (up to 7%) – the ability of soil to retain water
“It was an exciting surprise to see the degree of these changes over just a decade or so,” said Marshall McDaniel, associate professor of agronomy at Iowa State, who coordinated the study team. “It has been thought that it would take much longer to see some of these levels of change. Especially soil organic matter and maximum water-holding capacity”
Some measures continued to improve
Aggregate stability and maximum water-holding capacity increased throughout the study period. The increases in microbial biomass and soil organic matter plateaued over time, with the microbial biomass decreasing slightly at the end of the study period.
The study used a “paired chronoscope” approach to measure the changes. This “space-for-time” substitution used 15 paired control and treatment sites that were in prairie strips from 2- 13 years old and represented four of Iowa’s seven major landforms. Each pair had a prairie strip treatment and a cropland control managed in a conventional corn-soybean rotation. Most of the study sites were on private farmland. Six aspects of soil health were measured in the top six inches of the soil.
A more comprehensive assessment of soil health was conducted along the oldest (12-year-old) prairie strip at the Neal Smith National Wildlife Refuge near Prairie City. This research component was led by Elizabeth Riecke, a scientist with the Soil Health Institute, as part of its North American Project to Evaluate Soil Health Measurements.
Source : iastate.edu