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<title>Papers in Natural Resources </title>
<copyright>Copyright (c) 2009 University of Nebraska - Lincoln All rights reserved.</copyright>
<link>http://digitalcommons.unl.edu/natrespapers</link>
<description>Recent documents in Papers in Natural Resources </description>
<language>en-us</language>
<lastBuildDate>Sat, 14 Nov 2009 23:17:49 PST</lastBuildDate>
<ttl>3600</ttl>


	

	




<item>
<title>Geochemical Evidence for an Eolian Sand Dam across the North and South Platte Rivers in Nebraska</title>
<link>http://digitalcommons.unl.edu/natrespapers/176</link>
<guid isPermaLink="true">http://digitalcommons.unl.edu/natrespapers/176</guid>
<pubDate>Fri, 13 Nov 2009 11:20:34 PST</pubDate>
<description>Geochemical and geomorphic data from dune fields in southwestern
Nebraska provide new evidence that the Nebraska Sand
Hills once migrated across the North and South Platte rivers and
dammed the largest tributary system to the Missouri River. The
Lincoln County and Imperial dune fields, which lie downwind of
the South Platte River, have compositions intermediate between
the Nebraska Sand Hills (quartz-rich) and northeastern Colorado
dunes (K-feldspar-rich). The most likely explanation for the intermediate composition is that the Lincoln County and Imperial
dunes are derived in part from the Nebraska Sand Hills and in
part from the South Platte River. The only mechanism by which
the Nebraska Sand Hills could have migrated this far south is by
complete infilling of what were probably perennially dry North
Platte and South Platte river valleys. Such a series of events would
have required an extended drought, both for activation of eolian
sand and decreased discharges in the Platte River system. A
nearby major tributary of the North Platte River is postulated to
have been blocked by eolian sand about 12,000 14C yr B.P. We
propose that an eolian sand dam across the Plattes was constructed
at about this same time.</description>

<author>Daniel R. Muhs</author>


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<title>Late Holocene Eolian Activity in the Mineralogically Mature Nebraska Sand Hills</title>
<link>http://digitalcommons.unl.edu/natrespapers/175</link>
<guid isPermaLink="true">http://digitalcommons.unl.edu/natrespapers/175</guid>
<pubDate>Fri, 13 Nov 2009 11:15:49 PST</pubDate>
<description>The age of sand dunes in the Nebraska Sand Hills has been
controversial, with some investigators suggesting a full glacial age
and others suggesting that they were last active in the late Holocene.
New accelerator mass spectrometry radiocarbon ages of unaltered bison bones and organic rich sediments suggest that eolian
sand deposition occurred at least twice in the past 3000 I4C yr
B.P. in three widely separated localities and as many as three
times in the past 800 14C yr at three other localities. These late
Holocene episodes of eolian activity are probably the result of
droughts more intense than the 1930s &#34;Dust Bowl&#34; period, based
on independent Great Plains climate records from lake sediments
and tree rings. However, new geochemical data indicate that the
Nebraska Sand Hills are mineralogically mature. Eolian sands in
Nebraska have lower K feldspar (and K2O, Rb, and Ba) contents
than most possible source sediments and lower K-feldspar contents
than dunes of similar age in Colorado. The most likely explanation
for mineralogical maturity is reduction of sand sized K feldspar
to silt-sized particles via ballistic impacts due to strong winds over
many cycles of eolian activity. Therefore, dunes of the Nebraska
Sand Hills must have had a long history, probably extending over
more than one glacial-interglacial cycle, and the potential for
reactivation is high, with or without a future greenhouse warming.</description>

<author>Daniel R. Muhs</author>


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<title>Characterizing the Seasonal Dynamics of Plant Community Photosynthesis Across a Range of Vegetation Types</title>
<link>http://digitalcommons.unl.edu/natrespapers/174</link>
<guid isPermaLink="true">http://digitalcommons.unl.edu/natrespapers/174</guid>
<pubDate>Tue, 20 Oct 2009 13:49:42 PDT</pubDate>
<description>The seasonal cycle of plant community photosynthesis is one of the most important biotic oscillations to mankind. This study built upon previous efforts to develop a comprehensive framework to studying this cycle systematically with eddy covariance flux measurements. We proposed a new function to represent the cycle and generalized a set of phenological indices to quantify its dynamic characteristics. We suggest that the seasonal variation of plant community photosynthesis generally consists of five distinctive phases in sequence each of which results from the interaction between the inherent biological and ecological processes and the progression of climatic conditions and reflects the unique functioning of plant community at different stages of the growing season. We applied the improved methodology to seven vegetation sites ranging from evergreen and deciduous forests to crop to grasslands and covering both cool-season (vegetation active during cool months, e.g. Mediterranean climate grasslands) and warm-season (vegetation active during warm months, e.g. temperate and boreal forests) vegetation types. Our application revealed interesting phenomena that had not been reported before and pointed to new research directions. We found that for the warm-season vegetation type, the recovery of plant community photosynthesis at the beginning of the growing season was faster than the senescence at the end of the growing season while for the coolseason vegetation type, the opposite was true. Furthermore, for the warm-season vegetation type, the recovery was closely correlated with the senescence such that a faster photosynthetic recovery implied a speedier photosynthetic senescence and vice versa. There was evidence that a similar close correlation could also exist for the cool-season vegetation type, and furthermore, the recovery-senescence relationship may be invariant between the warm-season and cool-season vegetation types up to an offset in the intercept. We also found that while the growing season length affected how much carbon dioxide could be potentially assimilated by a plant community over the course of a growing season, other factors that affect canopy photosynthetic capacity (e.g. nutrients, water) could be more important at this time scale. These results and insights demonstrate that the proposed method of analysis and system of terminology can serve as a foundation for studying the dynamics of plant community photosynthesis and such studies can be fruitful.</description>

<author>Lianhong Gu</author>


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<item>
<title>Albedo estimates for land surface models and support for a new paradigm based on foliage nitrogen concentration</title>
<link>http://digitalcommons.unl.edu/natrespapers/173</link>
<guid isPermaLink="true">http://digitalcommons.unl.edu/natrespapers/173</guid>
<pubDate>Tue, 20 Oct 2009 13:31:25 PDT</pubDate>
<description>Vegetation albedo is a critical component of the Earth's climate system, yet efforts to evaluate and
improve albedo parameterizations in climate models have lagged relative to other aspects of
model development. Here, we calculated growing season albedos for deciduous and evergreen
forests, crops, and grasslands based on over 40 site-years of data from the AmeriFlux network and
compared them with estimates presently used in the land surface formulations of a variety of
climate models. Generally, the albedo estimates used in land surface models agreed well with
this data compilation. However, a variety of models using fixed seasonal estimates of albedo
overestimated the growing season albedo of northerly evergreen trees. In contrast, climatemodels
that rely on a common two-stream albedo submodel provided accurate predictions of boreal
needle-leaf evergreen albedo but overestimated grassland albedos. Inverse analysis showed that
parameters of the two-stream model were highly correlated. Consistent with recent observations
based on remotely sensed albedo, the AmeriFlux dataset demonstrated a tight linear relationship
between canopy albedo and foliage nitrogen concentration (for forest vegetation: albedo
 = 0.01 + 0.071%N, r2  = 0.91; forests, grassland, and maize: albedo = 0.02 + 0.067%N, r2 = 0.80).
However, this relationship saturated at the higher nitrogen concentrations displayed by soybean
foliage. We developed similar relationships between a foliar parameter used in the two-stream
albedo model and foliage nitrogen concentration. These nitrogen-based relationships can serve as
the basis for a new approach to land surface albedo modeling that simplifies albedo estimation
while providing a link to other important ecosystem processes.</description>

<author>David Y. Hollinger</author>


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<title>Nutrient Uptake and Mineralization during Leaf Decay in Streams - A Model Simulation</title>
<link>http://digitalcommons.unl.edu/natrespapers/172</link>
<guid isPermaLink="true">http://digitalcommons.unl.edu/natrespapers/172</guid>
<pubDate>Tue, 20 Oct 2009 13:13:17 PDT</pubDate>
<description>We developed a stoichiometrically explicit computer model to examine how heterotrophic uptake of nutrients and microbial mineralization occurring during the decay of leaves in streams may be important in modifying nutrient concentrations. The simulations showed that microbial uptake can substantially decrease stream nutrient concentrations during the initial phases of decomposition, while mineralization may produce increases in concentrations during later stages of decomposition. The simulations also showed that initial nutrient content of the leaves can affect the stream nutrient concentration dynamics and determine whether nitrogen or phosphorus is the limiting nutrient. Finally, the simulations suggest a net retention (uptake &gt; mineralization) of nutrients in headwater streams, which is balanced by export of particulate organic nutrients to downstream reaches. Published studies support the conclusion that uptake can substantially change stream nutrient concentrations. On the other hand, there is little published evidence that mineralization also affects nutrient concentrations. Also, there is little information on direct microbial utilization of nutrients contained in the decaying leaves themselves. Our results suggest several directions for research that will improve our understanding of the complex relationship between leaf decay and nutrient dynamics in streams.</description>

<author>J. R. Webster</author>


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<item>
<title>Probabilistic movement model with emigration simulates movements of deer in Nebraska, 1990-2006</title>
<link>http://digitalcommons.unl.edu/natrespapers/171</link>
<guid isPermaLink="true">http://digitalcommons.unl.edu/natrespapers/171</guid>
<pubDate>Tue, 20 Oct 2009 13:04:20 PDT</pubDate>
<description>Movements of deer can affect population dynamics, spatial redistribution, and transmission and spread
of diseases. Our goal was to model the movement of deer in Nebraska in an attempt to predict the potential
for spread of chronic wasting disease (CWD) into eastern Nebraska. We collared and radio-tracked
&#62;600 white-tailed deer (Odocoileus virginianus) and mule deer (Odocoileus hemionus) in Nebraska during
1990-2006.We observed large displacements (&#62;10 km) for both species and sexes of deer, including
migrations up to 100 km and dispersals up to 50 km. Average distance traveled between successive daily
locations was 166m for male and 173 for female deer in eastern Nebraska, and 427m for male and 459
for female deer in western Nebraska. Average daily displacement from initial capture point was 10m
for male and 14m for female deer in eastern Nebraska, and 27m for male and 28m for female deer in
western Nebraska.We used these data on naturally occurring movements to create and test 6 individual-based
models of movement for white-tailed deer and mule deer in Nebraska, including models that
incorporated sampling from empirical distributions of movement lengths and turn angles (DIST), correlated
random walks (CRW), home point fidelity (FOCUS), shifting home point (SHIFT), probabilistic
movement acceptance (MOVE), and probabilistic movement with emigration (MOVEwEMI). We created
models in sequence in an attempt to account for the shortcomings of the previous model(s). We used the
Kolmogrov-Smirnov goodness-of-fit test to verify improvement of simulated annual displacement distributions
to empirical displacement distributions. The best-fit model (D = 0.07 and 0.08 for eastern and
western Nebraska, respectively) included a probabilistic-movement chance with emigration (MOVEwEMI)
and resulted in an optimal daily movement length of 350m (maximum daily movement length of 2800m
for emigrators) for eastern Nebraska and 370m (maximum of 2960m) for western Nebraska. The proportion
of deer that moved as emigrators was 0.10 and 0.13 for eastern and western Nebraska, respectively.
We propose that the observed spread of CWD may be driven by large movements of a small proportion
of deer that help to establish a low prevalence of the disease in areas east of the current endemic area.
Our movement models will be used in a larger individual-based simulation of movement, survival, and
transmission of CWD to help determine future surveillance and management actions.</description>

<author>Charles J. Frost</author>


</item>


<item>
<title>Coyote Food Habits at DeSoto National Wildlife Refuge, Nebraska</title>
<link>http://digitalcommons.unl.edu/natrespapers/170</link>
<guid isPermaLink="true">http://digitalcommons.unl.edu/natrespapers/170</guid>
<pubDate>Tue, 20 Oct 2009 12:50:48 PDT</pubDate>
<description>Coyote (Canis latrans) food habits were detennined from 490
scats collected from October 1994 to October 1995 at DeSoto National
Wildlife Refuge (DNWR), along the Nebraska/Iowa border. Mammals
occurred most frequently, as measured by percent-of-scats (POS) , followed
by vegetation, birds, and invertebrates. Mammals also constituted the largest
portion of coyote diet, as determined by fresh weight correction factors. Within
the mammalian category, white-tailed deer (Odocoileus virginianus) occurred
most frequently and constituted the largest portion of diet by fresh weight
correction factors. White-tailed deer occurrence and importance in diet
peaked in June, which corresponds to the fawning period of white-tailed deer
at DNWR. Mammals occurred in greater than 75 POS in all months except
July and August, when mammals occurred in 38 and 30 POS, respectively.
In July and August, vegetation in coyote scats, primarily mulberries (Morus
spp.), was highest at 88 and 83 POS, respectively. Invertebrate occurrence
peaked in May and in September. Bird occurrence peaked in December,
which corresponded with the snow goose (Chen caerulescens) migration, and
May, which corresponded with the nesting period for several species of ground
nesting birds.</description>

<author>Jeffrey J. Huebschman</author>


</item>


<item>
<title>Reproductive Success of Grasshopper Sparrows in Relation to Edge</title>
<link>http://digitalcommons.unl.edu/natrespapers/169</link>
<guid isPermaLink="true">http://digitalcommons.unl.edu/natrespapers/169</guid>
<pubDate>Tue, 20 Oct 2009 12:45:08 PDT</pubDate>
<description>Using an index based on observations of breeding behaviors,
we estimated reproductive success of 31 territorial grasshopper sparrows
(Ammodramus savannarum) on Conservation Reserve Program fields in
southeast Nebraska. Reproductive success was 52%, and no difference was
detected between birds holding interior (&#62;100 m from the edge) vs. edge
territories. However, grasshopper sparrows appeared to avoid nesting within
50 m of edge habitats. Territories ranged from 0.36-1.24 ha, and territory
size did not differ between successful and unsuccessful males.</description>

<author>Jennifer M. DeLisle</author>


</item>


<item>
<title>Tree canopy effect on grass and grass/legume mixtures in eastern Nebraska</title>
<link>http://digitalcommons.unl.edu/natrespapers/168</link>
<guid isPermaLink="true">http://digitalcommons.unl.edu/natrespapers/168</guid>
<pubDate>Tue, 20 Oct 2009 12:40:37 PDT</pubDate>
<description>A study to determine the feasibility of
producing forage for grazing livestock under trees was
conducted as a step toward evaluating the potential for
silvopasture systems in the northern and central Great
Plains. The effects of overstory leaf area index (LAI),
percentage understory light transmittance (LT), and
soil moisture (SM) on yield and crude protein (CP) of
big bluestem [Andropogon gerardii Vitman; (BB)],
smooth bromegrass [ Bromus inermis  Leyss.; (SB)],
and mixtures with birdsfoot trefoil [ Lotus corniculatus
L.; (BFT)] were examined. The study was conducted in
both Scotch pine (Pinus sylvestris  L.) and green ash
(Fraxinus pennsylvancia  Marsh.) tree plantations, at
the University of Nebraska Agriculture Research and
Development Center near Mead, Nebraska. Thirty-six
plots representing a wide range of canopy cover were
selected at each location and seeded in April 2000 to
BB, SB, or mixtures with BFT. Measurements of LAI,
LT, and SM were taken throughout the 2001-growing
season and plots were harvested in June and September
2001. Soil moisture generally did not explain much of
the variability in yield or CP for BB, SB, or BFT.
Cumulative LAI or LT averaged over the growing
season was the best predictor of yield or CP, particularly
under the pine. Yields of BB and SB increased as
LAI decreased or LT increased. Conversely, the CP of
BB and SB increased as LT decreased for both the June
and September harvests. Both BB and SB maintain
relatively high productivity under partial shading;
however, BFT yields were low at LT levels below75%.</description>

<author>Michael El. L. Perry</author>


</item>


<item>
<title>Teaching Vertebrate Pest Control: A Challenge to Wildlife Professionals</title>
<link>http://digitalcommons.unl.edu/natrespapers/167</link>
<guid isPermaLink="true">http://digitalcommons.unl.edu/natrespapers/167</guid>
<pubDate>Tue, 22 Sep 2009 13:27:57 PDT</pubDate>
<description>Vertebrate pest control deals with wild animals that create health hazards, damage resources, or become a general nuisance. Some people prefer the terms &quot;wildlife damage control&quot; or &quot;animal damage control&quot; because they focus on controlling damage rather than controlling animals. This is an important principle. Vertebrate animals that cause damage often have many positive values. In dealing with these situations our objective should always be to reduce or prevent damage; this does not necessarily require the killing of animals. I use the term &quot;vertebrate pest control&quot; because I believe it is less ambiguous than &quot;damage control.&quot; When I call an animal a &quot;pest,&quot; I do so realizing this is a subjective term, and another person may have a different opinion.</description>

<author>Robert M. Timm</author>


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