Effects of golf course management on subsurface soil properties in Iowa
Author:
Streeter Matthew T.ORCID, Schilling Keith E.
Abstract
Abstract. Currently, in the USA and especially in the Midwest region, urban expansion
is developing turfgrass landscapes surrounding commercial sites, homes, and
recreational areas on soils that have been agriculturally managed for
decades. Often, golf courses are at the forefront of conversations concerning
anthropogenic environmental impacts as they account for some of the most
intensively managed soils in the world. Iowa golf courses provide an ideal
location to evaluate whether golf course management is affecting the quality
of soils at depth. Our study evaluated how soil properties relating to soil
health and resiliency varied with depth at golf courses across Iowa and
interpreted relationships of these properties to current golf course
management, previous land use, and inherent soil properties. Systematic
variation in soil properties including sand content, NO3, and soil organic matter (SOM) were
observed with depth at six Iowa golf courses among three landform regions.
Variability in sand content was identified between the 20 and 50 cm depth
classes at all courses, where sand content decreased by as much as 37 %.
Highest concentrations of SOM and NO3 were found in the shallowest
soils, whereas total C and P variability was not related to golf course
management. Sand content and NO3 were found to be directly related to
golf course management, particularly at shallow depths. The effects of golf
course management dissipated with depth and deeper soil variations were
primarily due to natural geologic conditions. The two abovementioned soil properties were very noticeably altered by golf course management and may directly impact
crop productivity, soil health, and water quality, and while NO3 may be
altered relatively quickly in soil through natural processes, particle size
of the soil may not be altered without extensive mitigation. Iowa golf
courses continue to be developed in areas of land use change from historically
native prairies and more recently agriculture to urban landscapes. As soils
are continually altered by human impacts, it is imperative that we monitor
the changes, both physical and chemical, in order to establish management
practices that maintain environmental sustainability and productivity.
Publisher
Copernicus GmbH
Reference36 articles.
1. Anderson, D., Saggar, S., Bettany, J., and Stewart, J.: Particle size
fractions and their use in studies of soil organic matter: I. The nature and
distribution of forms of carbon, nitrogen, and sulfur, Soil Sci. Soc. Am. J.,
45, 767–772, 1981. 2. Arya, L. M. and Paris, J. F.: A physicoempirical model to predict the soil
moisture characteristic from particle-size distribution and bulk density
data, Soil Sci. Soc. Am. J., 45, 1023–1030, 1981. 3. Balogh, J. C. and Walker, W. J.: Golf course management & construction:
Environmental issues, CRC Press, Boca Raton, FL, USA, 1992. 4. Bandaranayake, W., Qian, Y., Parton, W., Ojima, D., and Follett, R.:
Estimation of soil organic carbon changes in turfgrass systems using the
CENTURY model, Agron. J., 95, 558–563, 2003. 5. Bauters, T., Steenhuis, T., DiCarlo, D., Nieber, J., Dekker, L., Ritsema, C.,
Parlange, J.-Y., and Haverkamp, R.: Physics of water repellent soils, Journal
of Hydrology, 231, 233-243, 2000.
Cited by
1 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|