Monthly soil water content measurements measurements are made at 10
depths (where possible) at each of 10 probe access tubes at each of
the 15 plant NPP sites. The 10 probe access tubes at each site are
paired on each of the four sides and in the middle of the 70m x 70m
area used for long term plant NPP measurements. At the time of access
tube installation (aluminum 2 inch diameter irrigation pipe), the
pairing consisted of an access tube inserted vertically into the
ground midway under a shrub canopy of the dominant species and one
between shrubs. For grass dominated habitats, an access tube was
installed in the middle of the dominant perennial grass with the
second in the bare area between grass patches. Changes in perennial
plant cover through mortality or establishment may have changed this
relationship for some access tubes over the years.
Measurements with the neutron hydroprobe are taken at 30cm, 60cm,
90cm, 120cm, 150cm, 180cm, 210cm, 240cm, 270cm, and 300cm when
possible or to the greatest depth to which the associated access tube
could be installed before hitting an impenetrable petrocalcic layer
(caliche). Periodic "case standard" measurements are also
taken with the probe for each measurement campaign. The hydroprobe
detector totals the returning thermalized neutrons over a 16 second
sample time. This raw count value is then substituted into the proper
regression equation to calculate cubic centimeters of water per cubic
centimeter of soil (volumetric water content - VWC). Values of VWC for
the deepest available depth at each access tube are not calculated
because the soil volume directly below the probe is greater, and
therefore biased, relative to shallower depths.
Initial calibration regression equations were derived for the LTER-I
Transect soil water content study and applied to the measurements at
the NPP sites. Between 2003 and 2007 individual site regressions were
developed by Mike Duniway to better represent the variation in
soil characteristics. All data since initiation of the study (1989)
have now been recalculated using the new equations. The raw counts
of thermalized neutrons have also been adjusted to account for drift
associated with the decay rate of the Americium 241/Beryllium used to
generated the neutrons.
This data package provides the adjusted neutron counts, calculated
VWC, and ancillary calibration information (the attached
"Duniway_and_Crossland_2016_NeutronMoisture_Meter_Calibration.pdf").
The raw neutron count hydroprobe data, field methods, and measurement
history are provided in a separate Jornada Basin LTER data package on
EDI (knb-lter-jrn.210013001).