The objective of this study was to determine whether there have been
changes in the structure and function of the surface (0-20cm) soil
system, the zone most affected by litter decomposition, which is
associated with the rapid movement of Mesquite (Prosopsis
glandulosa) from historical habitats (arroyo and playa fringe) into
recent habitats (grassland and dunes). Four sites were established
at the Jornada Basin in 1986. To compare across habitats, mesquite
soil was sampled at playa, coppice dune, arroyo/wash, and grassland
sites.
The soils were sampled in October 1986. At each habitat type
location (playa, arroyo, grassland and dune) soil samples were
collected from the mid canopy beneath six mesquite plants at two
depths (0-10 cm and 10-20 cm), using a bucket auger soil corer (7.5
cm diameter, 10 cm depth). The samples were placed in plastic bags,
stored in a portable cooler, and then transported to the
laboratories. These samples were later divided into subsamples for
root mass, soil moisture, and soil chemical analyses.
The gravimetric soil water content of the soil samples was
determined 2-4 days after soil sample collection. Samples used for
texture, pH, total organic C, total N, and total P analyses were air
dried in a glasshouse, ground to break up clay and caliche
aggregates, and passed through a 2-mm mesh sieve. N mineralization
and inorganic N analyses were made on field-moist soil. Total C was
determined by dry combustion following pretreatment with acid to
remove carbonates (Nelson and Sommers 1982). Inorganic C was
determined by gravimetric loss of CO2 (U.S. Salinity Laboratory
Staff 1954). Particle size distribution was determined by hydrometer
method following pretreatment in the disperant sodium
hexametaphosphate (Gee and Bauder 1986). Total N and P were
determined by Kjeldahl digestion block technique (Bremmer and
Mulvaney 1982). Soil NH4 and NO3 were extracted in a 2 N KCl
solution and analyzed using an automated salicylate procedure
(Technicon Industrial Method No. 329-74 W/N). Available P was
analyzed as NaHCO3 extractable PO4-P (Olsen and Sommers 1982). The N
mineralization potential was estimated using a batch incubation
procedure on freshly collected soil as described by Fisher et al.
(1987). Two sets of 25-g soil subsamples were incubated at 29C for 4
weeks. The moisture content was adjusted to 0.1 g g-1 (field
capacity) at weekly intervals. The soils were extracted with 2 N KCl
(Keeney and Nelson 1982) and NH4+ and NO3 were determined as above.
Net N mineralization was calculated as the net change in N occurring
from the beginning to the end of the incubation period. This study
was completed in October 1986.
References:
Bremner, J.M. and C.S. Mulvaney. 1982. Nitrogen--Total. In A.L.
Page, R.H. Miller, and D.R. Keeney (eds.). Methods of soil analysis.
Part 2 - Chemical and microbiological properties. Agronomy 9
(2):595-624. Am. Soc. of Agron., Madison, Wis.
Gee, G.W. and J.W. Bauder. 1986. Particle-size analysis. In: Page,
A.L., R.H. Miller, and D.R. Keeney (eds.) Methods of soil analysis.
Chemical and microbiological properties. Agron 9, American Society
of Agronomy, Madison, Wisconsin, pp 383-411.
Jenkins, M.B., R.A. Virginia, and W.M. Jarrell. 1988. Depth
distribution and seasonal populations of mesquite-nodulating
rhizobia in warm desert ecosystems. Soil Science Society of America
Journal 52(6):1644-1650.
Nelson, D.W. and L.E. Sommers. 1982. Total carbon, organic carbon,
and organic matter. In: Page, A.L., R.H. Miller, D.R. Keeney(eds.)
Methods of soil analysis. Chemical and microbiological properties.
Agron 9, American Society of Agronomy, Madison, Wisconsin, pp
539-579.
Olsen, S.R., and L.E. Sommers. 1982. Phosphorus. In A.L. Page, R.H.
Miller, and D. R. Keeney (eds.) Methods of soil analysis. Part 2-
Chemical and microbiological properties. Agronomy 9 (2): 403-430.
Am. Soc. of Agron., Madison, Wis.
Technicon Industrial Method No. 154-71 NH4+ analysed
colorimetrically (indophenol blue) alkaline phenol-hypochlorite
reaction
Technicon Industrial Method No. 100-70W/ NO3- analysed
colorimetrically (copper-cadmium reduction to nitrite---->diazo
cpd--->reddish purple azo dye)
U.S. Salinity Laboratory Staff. 1954. Methods for soil
characterization. p. 84-89. In L.A. Richards (ed.) Diagnosis and
improvement of saline and alkali soils. USDA Agric. Handbook 60 U.S.
Govt Print. Office, Washington, DC.
Virginia, R.A., W.M. Jarrell, W.G. Whitford, and D.W. Freckman.
1992. Soil biota and soil properties in the surface rooting zone of
mesquite (Prosopis glandulosa) in historical and recently
desertified Chihuahuan Desert habitats. Biology and Fertility of
Soils 14:90-98.
Supplemental files:
mdssnutr.dsd: This is an early metadata file from the Jornada LTER
archives that may have some useful information.