Research objectives and design:
Soil samples were collected at a variety of grassland and mesquite
habitats in the Jornada Basin in a survey of soil N availability.
The study objective was to develop hypotheses about
desertification processes that degrade grassland into mesquite
dominated ecosystems.
Soil samples were collected on May 12 and May 13, 1986 in 10 sites
total, 5 associated with mesquite (Prosopsis glandulosa) and 5
grassland or grass habitats. These sites include USDA Mesquite
Dunes (MD_USDA), USDA Between Dunes (BD_USDA), IBP Grama Grassland
(GG_IBP), USDA Grama Grassland (GG_USDA), LTER Arroyo Mesquite
(AM_LTER), LTER Fluff Grass (FG_LTER), LTER Grama Grassland
(GG_LTER), LTER Playa Mesquite (GG_LTER), USDA Sporobolus/
Gutierrezia (SG_USDA), USDA Mesquite Grassland (MG_USDA). Soil
samples were collected to 20 cm or to hard pan, whichever came
first. After collection soils were incubated for up to 28 weeks
and soil N mineralization was measured using a leaching incubation
procedure.
Sampling and incubation details
At Fluff grass LTER (FG LTER), which is on the lower grassland of
the LTER control transect, samples were collected from fluff grass
clumps. At the Grama grassland LTER (GG LTER) site, which is on
the upper grassland of the LTER control transect, samples were
collected from black grama clumps. At the Sporobolus/Gutierrezia
USDA site (SG USDA), which is located just SE of the IBP grassland
site, samples were collected from Sporobolus/Gutierrezia clumps.
Sporobolus and Gutierrezia were dominant plants, but mesquite was
observed to be increasing in this area. Located just SE of IBP
grassland site. At the other Grama grassland sites (GG USDA &
GG IBP), samples were collected within clumps of black grama. At
the Playa mesquite site (PM LTER), soils were mostly clay, but a
few samples were quite coarse and had a hardpan at 10-15 cm. At
arroyo mesquite (AM LTER) soil samples were generally loamy and
had no detectable hardpan. A few had hardpans at 10-15 cm. Depth
to hardpan at all sites, and additional location descriptions, are
given in the attached "DSD" file (see below) from
Jornada LTER’s metadata archives.
Nitrogen mineralization of soils was measured up to 28 weeks
following Stanford and Smith’s (1972) leaching incubation method.
Briefly, an incubation procedure was utilized to describe the
relationship between cumulative N and incubation periods.
Incubation continued for 28 weeks at 350 C, where mineralized
nitrogen was removed by leaching with 0.01 M CaCI2 at 0, 1 2, 4,
8, 12, 16, 20, 24, and 28-week intervals. The N value was then
estimated from the cumulative amounts of nitrogen mineralized
under these conditions. This data set contains the week of
analysis, sample number, site, and inorganic nitrogen (mg-N/kg-dry
soil).
References
Stanford, George, and S. J. Smith. "Nitrogen mineralization
potentials of soils." Soil Science Society of America Journal
36, no. 3 (1972): 465-472.
Supplemental files
JornadaStudy_395_grama_mesquite_leaching_mineralization_potential_dsd.txt:
This is a metadata file from the Jornada LTER archives that may
have some useful information.