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ARS Home » Plains Area » Las Cruces, New Mexico » Range Management Research » Research » Publications at this Location » Publication #130793
Title: EFFECTS OF PLANT REMOVALS ON SOIL SURFACE EROSION IN A CHIHUAHUAN DESERT SHRUBLAND

Author
item HUENNEKE, LAURA - NEW MEXICO STATE UNIV
item BUONOPANE, M. - NEW MEXICO STATE UNIV
item BOTHERN, L. - NEW MEXICO STATE UNIV
item Herrick, Jeffrey - Jeff

Submitted to: Ecological Society of America Abstracts
Publication Type: Abstract Only
Publication Acceptance Date: 7/1/2000
Publication Date: 8/6/2000
Citation: HUENNEKE, L.F., BUONOPANE, M., BOTHERN, L., HERRICK, J.E. EFFECTS OF PLANT REMOVALS ON SOIL SURFACE EROSION IN A CHIHUAHUAN DESERT SHRUBLAND. 85TH MEETING OF THE ECOLOGICAL SOCIETY OF AMERICA. 2000. ABSTRACT P. 290.

Interpretive Summary:

Technical Abstract: Humans are dramatically altering the patterns of biological diversity in semi-arid ecosystems worldwide, in particular by altering the relative abundance of different growth forms (shrubs vs. perennial grasses) and by reducing the numbers of species within growth forms. We are exploring the impact of reduced plant diversity in experimental plots of creosotebush (Larrea tridentata) shrubland at the Jornada Basin LTER site near Las Cruces, NM, USA. In 1995, eight treatments of varying severity of plant community alteration were imposed on 25m x 25m plots (six replicates of each treatment); treatments ranged from no removals to extreme simplification of the perennial community (one shrub species, one grass species, one succulent, etc.). These treatments have been maintained since 1995. We have monitored soil erosion and sediment movement within these plots since spring 1996 by collecting sediment in pans at the downslope edge of each plot. Fine materials (particle diameter <2mm) dominate total soil movement (by weight), although larger particles are transported in this system, especially during the summer-fall season of intense episodic rainfall. Fine particle movement is higher in shrub removal and grass removal treatments than in controls during some seasons, especially in the summer. No statistically significant differences were detected during other seasons. Location on the slope with respect to local channels or arroyos contributes significantly to variation in the amount of material moving within a plot, as does the nature of vegetative cover and soil surface characteristics in the immediate vicinity of a collecting pan. Our results suggest the relationship between plant community structure and soil erosion rates is best examined at the scale of local patches.