<?xml version="1.0" encoding="UTF-8"?><rss version="2.0"  xmlns:dc="http://purl.org/dc/elements/1.1/"><channel><title>New Publications Online From The USFS Southern Research Station</title><link>http://www.srs.fs.usda.gov/pubs/</link><description>20 newest publications from the US Forest Service, Southern Research Station with headquarters in Asheville, North Carolina.  http://www.srs.fs.usda.gov/pubs/</description><language>en-us</language><lastBuildDate>Fri, 20 Aug 2004 01:50:21 CDT</lastBuildDate>

<item>
	<title>
		Investigating habitat value to inform contaminant remediation options: approach	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30625	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30625	</guid>
	<description>
		<![CDATA[Habitat valuation methods are most often developed and used to prioritize candidate lands for conservation. In this study the intent of habitat valuation was to inform the decision-making process for remediation of chemical contaminants on specific lands or surface water bodies. Methods were developed to summarize dimensions of habitat value for six representative aquatic and terrestrial contaminated sites at the East Tennessee Technology Park (ETTP) on the US Department of Energy Oak Ridge Reservation in Oak Ridge, TN, USA. Several general valuation metrics were developed for three broad categories: site use by groups of organisms, site rarity, and use value added from spatial context. Examples of use value metrics are taxa richness, a direct measure of number of species that inhabit an area, complexity of habitat structure, an indirect measure of potential number of species that may use the area, and land use designation, a measure of the length of time that the area will be available for use. Measures of rarity included presence of rare species or communities. Examples of metrics for habitat use value added from spatial context included similarity or complementarity of neighboring habitat patches and presence of habitat corridors. More specific metrics were developed for groups of organisms in contaminated streams, ponds, and terrestrial ecosystems. For each of these metrics, cutoff values for high, medium, and low habitat value were suggested, based on available information on distributions of organisms and landscape features, as well as habitat use information. A companion paper describes the implementation of these habitat valuation metrics and scoring criteria in the remedial investigation for ETTP.]]>	</description>
	<pubDate>
		Fri, 15 Aug 2008 10:41:41 -0400	</pubDate>

        <dc:creator>
                Efroymson, Rebecca A.; Peterson, Mark J.; Welsh, Christopher J.; Druckenbrod, Daniel L.; Ryon, Michael G.; Smith, John G.; Hargrove, William W.; Giffen, Neil R.; Roy, W. Kelly; Quarles, Harry D.        </dc:creator>
        <dc:subject>
                habitat, ecological valuation, remediation, contaminated site        </dc:subject>
</item> 



<item>
	<title>
		Drought during canopy development has lasting effect on annual carbon balance in a deciduous temperate forest	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30621	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30621	</guid>
	<description>
		<![CDATA[<ul><li>Climate change projections predict an intensifying hydrologic cycle and an increasing frequency of droughts, yet quantitative understanding of the effects on ecosystem carbon exchange remains limited </li><li>Here, the effect of contrasting precipitation and soil moisture dynamics were evaluated on forest carbon exchange using 2 yr of eddy covariance and microclimate data from a 50-yr-old mixed oak woodland in northern Ohio, USA. </li><li>The stand accumulated 40% less carbon in a year with drought between bud-break and full leaf expansion (354 &#xb1; 81 g C m<sup>&#8722;2</sup> yr<sup>&#8722;1</sup> in 2004 and 252 &#xb1; 45 g C m<sup>&#8722;2</sup> yr<sup>&#8722;1</sup> in 2005). This was caused by greater suppression of gross ecosystem productivity (GEP; 16% = 200 g) than of ecosystem respiration (ER; 11% = 100 g) by drought. Suppressed GEP was traced to lower leaf area, lower apparent quantum yield and lower canopy conductance. The moisture sensitivity of ER may have been mediated by GEP.</li><li>The results highlight the vulnerability of the ecosystem to even a moderate drought, when it affects a critical aspect of development. Although the drought was preceded by rain, the storage capacity of the soil seemed limited to 1&#x96;2 wk, and therefore droughts longer than this are likely to impair productivity in the region.</li></ul>]]>	</description>
	<pubDate>
		Wed, 13 Aug 2008 14:49:02 -0400	</pubDate>

        <dc:creator>
                Noormets, Asko; McNulty, Steve G.; DeForest, Jared L.; Sun, Ge; Li, Qinglin; Chen, Jiquan        </dc:creator>
        <dc:subject>
                canopy conductance, canopy development, drought, ecosystem respiration (ER), gross ecosystem productivity (GEP), leaf expansion, net ecosystem exchange of carbon (NEE), rainfall distribution         </dc:subject>
</item> 



<item>
	<title>
		Nature-based outdoor recreation trends and wilderness	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30615	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30615	</guid>
	<description>
		<![CDATA[Wilderness and other public land management agencies, both federal and state, have been feeling a pinch. It seems this pinch may partly be in response to a growing perception, or perhaps misperception,that nature-based, especially wildland recreation, is on the decline. This perception has been getting a lot of media attention of late. Some of us who have done research about nature-based recreation trends for years wonder what the reaction to such a perception might be.]]>	</description>
	<pubDate>
		Thu, 07 Aug 2008 10:14:52 -0400	</pubDate>

        <dc:creator>
                Cordell, H. Ken; Betz, Carter, J.; Green, Gary T.        </dc:creator>
        <dc:subject>
                        </dc:subject>
</item> 



<item>
	<title>
		The latest trends in nature-based outdoor recreation	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30614	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30614	</guid>
	<description>
		<![CDATA[Considerable interest in better understanding current trends in nature-based
outdoor recreation followed publication of Richard Louv's book, Last Child
in the Woods, and a recent paper by Oliver R.W. Pergams and Patricia A.
Zaradic titled "Evidence for a Fundamental and Pervasive Shift away from Nature-Based Recreation."]]>	</description>
	<pubDate>
		Thu, 07 Aug 2008 09:44:44 -0400	</pubDate>

        <dc:creator>
                Cordell, H. Ken        </dc:creator>
        <dc:subject>
                        </dc:subject>
</item> 



<item>
	<title>
		Tree-ring model interprets growth decline in natural stands of loblolly pine in the southeastern United States	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30607	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30607	</guid>
	<description>
		<![CDATA[Annual ring widths and ring areas from 131 even-aged, natural, well-stocked stands of loblolly pine (Pinus taeda L.) in the Piedmont region were analyzed to reveal possible causes of a previously reported decline in radial growth. A linear aggregate model was used to separate independent factors that are known to contribute to radial growth variation in this species. Stand, site, and climatic conditions were reconstructed for each stand for the 36-year period 1949-1984 from previous inventories and from weather records at appropriately located stations. Within each of six 5-year age-classes, the model identified declines in both ring width and ring area associated with stand density, climate changes, and the passage of time. Regional climate first ameliorated this decline as pine stands passed from droughty conditions early in the 36-year period to a favorable climate during the middle of the period, and the decline accelerated later with the return of dry conditions toward the end of the period. The tree-ring model simulates a decline in radial increment in trees in natural pine stands between the ages of 20 &d 45 years in the Piedmont which has averaged 1% per year since 1950. Part of the downward trend was attributed to increased competition, part to regional drought, and-a considerable part to unidentified factors, possibly regional atmospheric deposition.]]>	</description>
	<pubDate>
		Tue, 05 Aug 2008 15:13:19 -0400	</pubDate>

        <dc:creator>
                Zahner, Robert; Saucier, Joseph R.; Myers, Richard K.        </dc:creator>
        <dc:subject>
                        </dc:subject>
</item> 



<item>
	<title>
		Moisture in untreated, a cetylated, and furfurylated Norway spruce studied during drying using time domain NMR	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30604	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30604	</guid>
	<description>
		<![CDATA[Using time domain NMR, the moisture in Norway spruce (<i>Picea abies</i> (L.) Karst.) sapwood subjected to four different treatments (never-dried, dried and remoistened, acetylated, and furfurylated) was studied during drying at 40°C, at sample average moisture contents above fiber saturation. Spin-spin relaxation time distributions were derived from CPMG relaxation curves using multiexponential fitting (CONTIN), and the resulting water populations were assigned according to the literature and their behavior during drying. It was found that both acetylation and furfurylation increased the average spinspin relaxation time of the lumen water in earlywood tracheids from about 80&#x96;100 ms to 200 and 300 ms, respectively. The average spin-spin relaxation time of the cell wall water was reduced from about 1.4 to 0.65 ms by furfurylation, while acetylation had less effect on this water. The relaxation times of both the earlywood lumen water and of the cell wall water were slightly longer for the never-dried samples than for the dried and remoistened samples.]]>	</description>
	<pubDate>
		Tue, 05 Aug 2008 14:26:27 -0400	</pubDate>

        <dc:creator>
                Thygesen, Lisabeth G.; Elder, Thomas        </dc:creator>
        <dc:subject>
                Time domain, NMR, spin-spin relaxation, wood, moisture, water, acetylation, furfurylation        </dc:subject>
</item> 



<item>
	<title>
		Genetic diversity within and among populations of shortleaf pine (Pinus echinata Mill.) and loblolly pine (Pinus taeda L.)	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30600	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30600	</guid>
	<description>
		<![CDATA[Shortleaf pine (n=93) and loblolly pine (n=112) trees representing 22 seed sources or 16 physiographic populations were sampled from Southwide Southern Pine Seed Source Study plantings located in Oklahoma, Arkansas and Mississippi. The sampled trees were grown from shortleaf pine and loblolly pine seeds formed in 1951 and 1952, prior to the start of intensive forest management across their native ranges. Amplification fragment length polymorphism (AFLP) markers were developed and used to study genetic diversity and its structure in these pine species. After screening 48 primer pairs, 17 and 21 pairs were selected that produced 794 and 647 AFLPs in shortleaf pine and loblolly pine, respectively. High-AFLP-based genetic diversity exists within shortleaf pine and loblolly pine, and most (84.73% in shortleaf pine; 87.69% in loblolly pine) of this diversity is maintained within physiographic populations. The high value of unbiased measures of genetic identity and low value of genetic distance for all pairwise comparisons indicates that the populations have similar genetic structures. For shortleaf pine, there was no significant correlation between geographic distance and genetic distance (r=0.28), while for loblolly pine there was a weak but significant correlation (r=0.51).]]>	</description>
	<pubDate>
		Tue, 05 Aug 2008 11:49:16 -0400	</pubDate>

        <dc:creator>
                Xu, Shiqin; Tauer, C.G.; Nelson, C. Dana        </dc:creator>
        <dc:subject>
                genetic diversity        </dc:subject>
</item> 



<item>
	<title>
		Natural hybridization within seed sources of shortleaf pine (Pinus echinata Mill.) and loblolly pine (Pinus taeda L.)	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30599	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30599	</guid>
	<description>
		<![CDATA[Shortleaf and loblolly pine trees (n=93 and 102, respectively) from 22 seed sources of the Southwide Southern Pine Seed Source Study plantings or equivalent origin were evaluated for amplified fragment length polymorphism (AFLP) variation. These sampled trees represent shortleaf pine and loblolly pine, as they existed across their native geographic ranges before intensive forest management. Using 17 primer pairs, a total of 96 AFLPs between shortleaf pine and loblolly pine were produced and scored on the sample trees and two control-pollinated F1 interspecies hybrids and their parents. In addition, the well known isocitrate dehydrogenase (IDH) isozyme marker was scored for all trees. IDH detected two putative hybrids among the loblolly pine samples and two among the shortleaf pine samples, while either 13 or 12 putative hybrids were detected using all AFLP markers and IDH and either New Hybrids or Structure software, respectively. Results of this study show that later generation hybrids can be reliably identified using AFLP markers and confirmed that IDH is not a definitive marker for detecting hybrids; that is, at least in some seed sources, the alternative species' IDH allele resides in the source species. Based on all the markers, hybridization frequency varied geographically, ranging from 30% in an Arkansas seed source to 0% in several other seed sources. The hybridization level was higher in populations west of the Mississippi River than in populations east of the river; the shortleaf pine hybridization rates were 16.3% and 2.4% and the loblolly pine rates were 4.5% and 3.3%, west and east of the river, respectively. The results suggest that hybridization between these two species is significant but varies by seed source and species, and the potential for the unintended creation of hybrids should be considered in forest management decisions regarding both natural and artificial regeneration.]]>	</description>
	<pubDate>
		Tue, 05 Aug 2008 11:25:54 -0400	</pubDate>

        <dc:creator>
                Xu, Shiqin; Tauer, C.G.; Nelson, C. Dana        </dc:creator>
        <dc:subject>
                Genetic diversity        </dc:subject>
</item> 



<item>
	<title>
		Forest inventory and management-based visual preference models of southern pine stands	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30597	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30597	</guid>
	<description>
		<![CDATA[Statistical models explaining students' ratings of photographs of within stand forest scenes were constructed for 99 forest inventory plots in east Texas pine and oak-pine forest types. Models with parameters that are sensitive to visual preference yet compatible with forest management and timber inventories are presented. The models suggest that the density of sawtimber-sized trees and the proportion of visual penetration are positively associated with scenic beauty. Foliage, twig, and small stem screening, and the density of small-diameter trees are negatively associated with scenic beauty. Results generally concur with other visual preference studies of within-stand forest scenes. Such models and associated parameter estimates can be used to objectively assess within-stand forest scenes and to routinely monitor scenic beauty of southern pine forest resources. Unlike similar scenic beauty studies, the limited amount of downed wood encountered was positively associated with scenic beauty. Also suggested is a decline in perceived scenic beauty during the summer season (May-October) coincident with sampling from northeast to southwest sections of east Texas.]]>	</description>
	<pubDate>
		Thu, 31 Jul 2008 13:51:07 -0400	</pubDate>

        <dc:creator>
                Rudis, Victor A.; Gramann, James H.; Ruddell, Edward J.; Westphal, Joanne M.        </dc:creator>
        <dc:subject>
                Scenic beauty estimation, scenic quality, multiresource forest inventories, vegetative screening, within-season change, regional change        </dc:subject>
</item> 



<item>
	<title>
		Screenometer: a device for sampling vegetative screening in forested areas	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30596	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30596	</guid>
	<description>
		<![CDATA[A-device for estimating the degree to which vegetation and other obstructions screen forested areas has been adapted to an extensive sampling design for forest surveys. Procedures are recommended to assure that uniform measurements can be made. Examination of sources of sampling variation (observers, points within sampled locations, series of observations within points, and sectors within series) and sampling intensity suggests a sample design which involves a combination of points and sectors.]]>	</description>
	<pubDate>
		Thu, 31 Jul 2008 13:48:19 -0400	</pubDate>

        <dc:creator>
                Rudis, Victor A.        </dc:creator>
        <dc:subject>
                        </dc:subject>
</item> 



<item>
	<title>
		Forest-range resources of Southwest Louisiana	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30595	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30595	</guid>
	<description>
		<![CDATA[Findings of the first forest-range inventory of southwest Louisiana conducted as part of the nationwide Forest Survey are described and evaluated. Measurements indicate that the grazing potential of the region's forest ranges is not being fully used. Little competition with wildlife populations and timber stands is indicated at existing levels of understory utilization by livestock]]>	</description>
	<pubDate>
		Thu, 31 Jul 2008 11:36:33 -0400	</pubDate>

        <dc:creator>
                Sternitzke, Herbert S.; Pearson, Henry A.        </dc:creator>
        <dc:subject>
                        </dc:subject>
</item> 



<item>
	<title>
		Botanical composition and nutritive value of cattle diets on southern pine range	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30594	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30594	</guid>
	<description>
		<![CDATA[The botanical composition of the cattle diet and the nutritive value of about 50 herbaceous and woody diet components are sampled and reparted for the longleaf pine-bluestem range in Louisiana. Digestibility is also related to the diet.]]>	</description>
	<pubDate>
		Thu, 31 Jul 2008 11:31:54 -0400	</pubDate>

        <dc:creator>
                Pearson, H.A.; Grelen, H.E.; Epps, E.A.; Johnson, M.K.; Blakewood, B.W.        </dc:creator>
        <dc:subject>
                        </dc:subject>
</item> 



<item>
	<title>
		Forest area estimates from landsat MSS And forest inventory plot data	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30593	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30593	</guid>
	<description>
		<![CDATA[Provides details of an area that probably represents a natural ecological succession relatively undisturbed by man. The area includes unique vegetative types.]]>	</description>
	<pubDate>
		Thu, 31 Jul 2008 11:29:01 -0400	</pubDate>

        <dc:creator>
                Birdsey, Richard A.; Miller, W. Frank; Clark, Jon; Smith, Robert H.        </dc:creator>
        <dc:subject>
                        </dc:subject>
</item> 



<item>
	<title>
		An eco-hydrological project on Turkey Creek watershed, South Carolina, U.S.A.	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30592	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30592	</guid>
	<description>
		<![CDATA[The low-gradient, forested wetland landscape of the southeastern United States' Coastal Plain represents an important eco-hydrologic system, yet there is a very little information available on the region's ecological, hydrological and biogeochemical processes. Long-term hydrologic monitoring can provide the information needed to understand basic hydrologic processes and their interactions with climatic variation, ecosystem processes, land use change, and other natural and anthropogenic disturbances. Monitoring also provides researchers with baseline data for evaluating responses, generating new scientific hypotheses, and testing eco-hydrologic models. This information is crucial for the sustainable management of present and future water resources in the southeastern Coastal Plain region, with its growing population, rapidly expanding development, and intensive timber and agricultural industries. This paper presents a multi-collaborative approach for building a monitoring and modeling framework for conducting long-term eco-hydrological studies on a 5,000 ha watershed in the South Carolina Coastal Plain. ]]>	</description>
	<pubDate>
		Wed, 30 Jul 2008 14:34:26 -0400	</pubDate>

        <dc:creator>
                Amatya, Devendra; Trettin, Carl        </dc:creator>
        <dc:subject>
                Low-gradient, Coastal plain, forested wetlands, water management, water quality, monitoring, modeling, Francis Marion National Forest        </dc:subject>
</item> 



<item>
	<title>
		Development of watershed hydrologic research at Santee Experimental Forest, coastal South Carolina	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30591	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30591	</guid>
	<description>
		<![CDATA[Managing forested wetland landscapes for water quality improvement and productivity requires a detailed understanding of functional linkages between ecohydrological processes and management practices. Watershed studies are being conducted at USDA Forest Service Santee Experimental Forest, South Carolina, to understand the fundamental hydrologic and biogeochemical processes and their linkages with soils, vegetation, topography, climate, and management practices in the low gradient forested landscapes of the South Carolina Coastal Plain. This study presents an overview of and builds on the long-term watershed hydrologic research begun in 1964 by our predecessors at this experimental forest. Monitoring and modeling studies using a paired watershed approach are being conducted to describe the effects of management practices on two first-order, forested watersheds. Long-term flow data from two 160-ha first-order, one 500-ha second-order, and one 4,500-ha third-order watersheds, provide an opportunity to evaluate the flow dynamics and hydrologic effects of scale, land use distribution, and climate on these coastal watersheds. DRAINMOD-based models are being tested with these data for their applicability as a water management tool on these poorly drained natural forested watersheds. The long-term information on hydro-meteorology, water quality and water table levels from these watersheds has also provided baseline data on the ecohydrologic processes that are useful to researchers, planners, land owners and industries for the assessment of land management and climatic impacts. Such information for poorly drained low gradient coastal watersheds is becoming increasingly important for sustainable development as population pressure and timber demand continue to rise in the southeastern United States.]]>	</description>
	<pubDate>
		Wed, 30 Jul 2008 12:37:27 -0400	</pubDate>

        <dc:creator>
                Amatya, Devendra; Trettin, Carl         </dc:creator>
        <dc:subject>
                poorly drained soils, forested wetlands, forest management, outflow (runoff ), water budget, water quality, hydrologic modeling, DRAINMOD        </dc:subject>
</item> 



<item>
	<title>
		Flow dynamics of three experimental forested watersheds in coastal South Carolina (USA)	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30590	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30590	</guid>
	<description>
		<![CDATA[Three first-, second- and third-order experimental forested watersheds located within the Francis Marion National Forest in the lower coastal plain of South Carolina were monitored for rainfall and stream outflows. The largest watershed (WS 78) with some open lands, roads and wetlands gave higher annual water yields compared to the two other smaller ones (WS 79, WS 80) with mostly forest vegetation, possibly due to a difference in land
use, soils and topography as well as increased base flows. Flow duration curves yielded largest flow rates exceeding 4% of the time for the second-order watershed (WS 79). As expected, the daily flows persisted for 79% of the time in the largest 3rd-order watershed (WS 78) with a larger storage compared to only 65 and 60% in the 2nd- and 1st-order watersheds. The flow frequency analysis of peak flows, employing Pearson III-type distribution, revealed the peak flows for 100-, 50-, 25-, 10- and 5-year return periods as 1805, 1565, 1326, 1009 and 769 cfs (cubic feet per second) for WS 78; 379, 325, 272, 200 and 146 cfs for WS 79; and 73, 63, 54, 41 and 32 cfs for WS 80. These results are in good agreement with the data calculated using the USGS-developed formulae for the South Carolina
Lower Coastal Plain and have implications for the design of engineering structures, water and nutrient management, as well as evaluation of the impacts of development and natural disturbances on the forested lands of the Atlantic Coastal Plain.]]>	</description>
	<pubDate>
		Wed, 30 Jul 2008 07:56:21 -0400	</pubDate>

        <dc:creator>
                Amatya, Devendra M.; Radecki-Pawlik, Artur        </dc:creator>
        <dc:subject>
                        </dc:subject>
</item> 



<item>
	<title>
		Effects of drainage and forest management practices on hydraulic conductivity of wetland soils	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30589	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30589	</guid>
	<description>
		<![CDATA[Continuous records of water table elevations and flow rates from drained forested lands were analysed to determine field effective hydraulic conductivity (K) of a mineral (Deloss s.l.) and an organic (Belhaven muck)
soil. K of the top 90 cm of Deloss under mature pine was 60 m/day, which is 20 to 30 times that published for this series. Harvest had a minor effect on K, but site preparation for regeneration, including bedding, reduced the effective K to values typically assumed for this series, 3.6 m/d for the top 45 cm and 1.6 m/d for deeper layers. After regeneration, K values had nearly returned to original values within 8 years after planting. Similar observations on organic soils indicated that field effective K in drained pine plantations is substantially higher than the same soil under agricultural production.]]>	</description>
	<pubDate>
		Wed, 30 Jul 2008 07:45:34 -0400	</pubDate>

        <dc:creator>
                Skaggs, R.W.; Chescheir, Amatya, D.M.; Diggs, J.D.         </dc:creator>
        <dc:subject>
                drainage, organic soils, hydraulic conductivity, water table, wetland forest        </dc:subject>
</item> 



<item>
	<title>
		The woody biomass resource of Alabama	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30588	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30588	</guid>
	<description>
		<![CDATA[Presents findings and analysis of woody biomass based on the fifth forest survey of Alabama (1982). The green weights by component-total, merchantable, residual, sapling, and rough and rotten-are presented by various categories such as ownership, forest type, physiographic class, size class, basal area, species, and age. After-harvest residual is also presented and discussed.]]>	</description>
	<pubDate>
		Tue, 29 Jul 2008 16:52:04 -0400	</pubDate>

        <dc:creator>
                Rosson, James F. Jr.; Thomas, Charles E.        </dc:creator>
        <dc:subject>
                biomass, green weight, merchantable weight, residual weight, harvesting, clearcut, basal area, forest ecosystem        </dc:subject>
</item> 



<item>
	<title>
		Economic impacts of current-use assessment of rural land in the east Texas pineywoods region	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30587	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30587	</guid>
	<description>
		<![CDATA[Those provisions of Texas law that authorize optional current-use property tax assessment for forest and other rural land were studied to: (1) estimate the extent of adoption by qualifying property owners, (2) estimate the effects on assessments and taxes of enrolled land, (3) estimate the impacts on revenues received by local units of government, (4) estimate the effects on taxes born by ineligible and nonparticipating property owners, and (5) evaluate the impacts on rural land use decisions. The study focused on the east Texas pineywoods region because of the continuing controversy that has surrounded the application of current-use assessment within this heavily timbered part of the State.]]>	</description>
	<pubDate>
		Tue, 29 Jul 2008 16:23:15 -0400	</pubDate>

        <dc:creator>
                Hickman, Clifford A.; Crowther, Kevin D.        </dc:creator>
        <dc:subject>
                forest economics, property taxation        </dc:subject>
</item> 



<item>
	<title>
		Rainfall-runoff modeling of the Chapel Branch Creek Watershed using GIS-based rational and SCS-CN methods	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30586	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30586	</guid>
	<description>
		<![CDATA[Chapel Branch Creek (CBC), located within the Town of Santee adjacent to Lake Marion in Orangeburg County, SC, is listed on the SC 2004 303(d) list of impaired waterbodies due to elevated levels of nitrogen (N), phosphorus (P), chlorophyll-a, and pH. In this study, using a GIS-based approach, two runoff modeling methods, the Rational and SCS-CN methods, have been applied to the (~1600 ha) CBC watershed to estimate both event storm runoff and
peak runoff rates. Rainfall intensities from five observed storms were used in the models together with the runoff coefficients and curve numbers (CN) for various land use categories obtained by digitizing (1:5000 scale) 2005 NAIP aerial photos of 1-m resolution. In order to test the models, results were compared to the observed peak flow rates and runoff for storm events
recorded at sampling location 7 (SL-7), which drains an area of ~583 ha within the watershed. Results of this study show that a weighted low C-value (Rational Method) and a weighted Q (SCS-CN method) yield the most accurate estimates of peak runoff rates. The peak rates estimated by the SCS-CN method were in better agreement with the observed data than the
Rational Method. In addition, both the estimated runoff depths and the peak flow rates were more accurate when aggregated by sub-unit within the catchment than when calculated for the whole drainage catchment using the SCS-CN method.]]>	</description>
	<pubDate>
		Tue, 29 Jul 2008 15:00:53 -0400	</pubDate>

        <dc:creator>
                Mihalik, Elizabeth N.; Levine, Norm S.; Amatya, Devendra M.         </dc:creator>
        <dc:subject>
                Hydrologic modeling, Peak runoff rate, Runoff depth, Curve Number, Runoff
Coefficient        </dc:subject>
</item> 



<item>
	<title>
		Hydrologic impacts of converting grassland to managed forestland in Uruguay	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30585	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30585	</guid>
	<description>
		<![CDATA[Over 500,000 hectares of grassland have been converted to managed forestland in Uruguay since 1990. This study was initiated to determine the hydrologic and water quality impacts of changing land use from grassland (pasture) to pine plantation in Uruguay. Two adjacent watersheds located on the El Cerro ranch in the Tacuarembo River basin were selected for a paired watershed study. Outflow rates and water table depths are continuously measured on each watershed. Rainfall and meteorological conditions are also measured continuously on the site. During the initial pretreatment period (July 01, 2000 through June 2003) both watersheds remained in pasture. One watershed (107 ha) was planted with loblolly pine Pinus teada L.) in July 2003, while the other (69 ha) remained in pasture. Data collected during the past 48 month period (July 01, 2003 through June 2007) represent the first four years of the treatment period. Significant changes in water yield were not observed during the first three years of the treatment period, but water yield reductions were observed during the fourth year. Most of the reductions were observed during a wet period that occurred after a prolonged dry period. Reductions in water yield occurred during storm flow events. Changes were not observed in the base flow from the watersheds. Peak flow rates from the forested land were only 25% of those observed before planting and the times to peaks were increased by 26
minutes. Data collection will continue through the growth cycle of the trees.]]>	</description>
	<pubDate>
		Tue, 29 Jul 2008 14:52:27 -0400	</pubDate>

        <dc:creator>
                Chescheira, G.M.; Skaggsa, R.W.; Amatyab, D.M.         </dc:creator>
        <dc:subject>
                Afforestation, Forest hydrology, Water yield, Paired watersheds, Loblolly pine        </dc:subject>
</item> 



<item>
	<title>
		A comprehensive bibliography on vacation homes and recreational lands in the United States	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30584	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30584	</guid>
	<description>
		<![CDATA[This bibliography contains 619 references on vacation homes and recreational lands. It is divided into five major parts: I-evolution of the markets. II-analyzing the markets. III-the consumer, IV-impacts from recreational properties, and V-miscellaneous.]]>	</description>
	<pubDate>
		Tue, 29 Jul 2008 14:52:18 -0400	</pubDate>

        <dc:creator>
                Ragatz, Richard L.; Cordell, H. Ken        </dc:creator>
        <dc:subject>
                Markets, land development, condominiums, recreational properties        </dc:subject>
</item> 



<item>
	<title>
		Hydrology of a natural hardwood forested wetland	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30583	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30583	</guid>
	<description>
		<![CDATA[This paper documents the hydrology of a natural forested wetland near Plymouth, NC, USA. The research site was located on one of the few remaining, undrained non-riverine, palustrine forested hardwood wetlands on the lower coastal plain of North Carolina. A 137 ha watershed within the 350ha wetland was selected for intensive field study. Water balance components including surface runoff, lateral seepage, soil air volume, rainfall, and evapotranspiration were monitored for a three year period. Water balance closure error over the 36 month period was 5%. The hydrology model DRAINMOD predicted that average annual outflow from the wetland would have been 23.3% of the average annual rainfall (1288 mm) during the 68 year period from 1933 to 2000.]]>	</description>
	<pubDate>
		Tue, 29 Jul 2008 14:44:28 -0400	</pubDate>

        <dc:creator>
                Chescheir, George M.; Amatya, Devendra M.; Skaggs, R. Wayne         </dc:creator>
        <dc:subject>
                water balance, DRAINMOD, flow duration curve        </dc:subject>
</item> 



<item>
	<title>
		Effects of thinning on hydrology and water quality of a drained pine forest in coastal North Carolina	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30582	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30582	</guid>
	<description>
		<![CDATA[A study was conducted to examine the effects of commercial thinning on hydrology and water quality of a 28-year old (in 2002) drained loblolly pine (Pinus taeda L.) plantation watershed (D3) using another adjacent watershed (D1) as a control. A paired watershed approach was used with data from two periods (1988-90 and 2000-02) for calibration and data from 2002-07 as the treatment period. Both of these 25 ha watersheds are located in Carteret County, North Carolina. Results showed a consistent rise in
water table elevations on D3 compared to the control during the six months after 50% thinning. The water table rise of 12.6 cm on average decreased substantially by June 2007, indicating an increase in evapotranspiration caused by increased canopy closure. Similarly, flow rates increased immediately after thinning and decreased soon thereafter. Monthly outflows on thinned watershed were generally higher in the summer-fall months compared to the control. However, the total annual outflow from the treatment was lower than the control, except for the very wet years of 2003 with extremely high rainfall (>2300 mm) and 2005, possibly indicating a hydrologic recovery due to canopy closure approximately three years after
thinning. Thinning did not affect nutrient concentrations and loading rates, except for NO3-N and total P. The increases in both of these nutrients were minor compared to the values obtained from fertilization of
these stands. Results of the study indicate thinning may have only a short term (up to three years) effect on hydrology and water quality of drained pine plantation.]]>	</description>
	<pubDate>
		Tue, 29 Jul 2008 14:36:57 -0400	</pubDate>

        <dc:creator>
                Amatya, D.M.; Skaggs, R.W.        </dc:creator>
        <dc:subject>
                Loblolly pine, Drainage Outflow, Evapotranspiration, Water Table, Nutrients        </dc:subject>
</item> 



<item>
	<title>
		Impacts of fertilizer additions on water quality of a drained
pine plantation in North Carolina. A worst case scenario.	</title>
	<link>
		http://www.srs.fs.usda.gov/pubs/30581	</link>
	<guid>
		http://www.srs.fs.usda.gov/pubs/30581	</guid>
	<description>
		<![CDATA[Intensive plantation forestry will be increasingly important in the next 50 years to meet the high demand for domestic wood in the US. However, forestry management practices can substantially influence downstream water quality and ecology. In this study, the effect of fertilization on drainage water quality of a coastal pine plantation located in Carteret County, NC was studied. The pine plantation consists of three watersheds, two mature (31-year old) and a young (8-year old)stands (age at treatment). One of the mature stands was commercially thinned in 2002. The unthinned mature stand was designated as a control and was not fertilized. The two other stands
(young and thinned) were fertilized with diammonium phosphate, urea, and boron. Each treatment watershed received a different fertilizer rate. Both the flow rates and nutrient concentrations in water drained from each of the watersheds were measured. Nutrient concentrations and nutrient loadings
were analyzed using a paired watershed approach and GLM statistical procedures. Three large storm events occurred soon after fertilization, a 5-year 24 hr, a 1 to 2-year, and a third event (46 mm in 46 hr) occurred six, 29 and 47 days after fertilization respectively. It was determined that peak nutrient concentrations soon after fertilization were much higher than the average concentrations, which were significantly (&#945; = 0.05) higher on both treatment watersheds soon after fertilization than during any other period during the study. The effect of fertilization on both the nutrient
concentrations and loading rates was short lived and the levels were back to pre-fertilization levels as soon as three months after fertilization. Also, the average nutrient increase on the thinned stand was higher than on the young stand as a result of a higher fertilizer rate applied on the thinned stand one.]]>	</description>
	<pubDate>
		Tue, 29 Jul 2008 14:26:34 -0400	</pubDate>

        <dc:creator>
                Beltran, Bray J.; Amatya, Devendra M.; Jones, Martin; Skaggs, R. Wayne; P.E. Reynolds, William Neal; Callahan, Timothy J.; Nettles, Jami E.        </dc:creator>
        <dc:subject>
                Drainage outflow, Nutrient Concentrations, Nutrient Loadings, Water Quality, Paired Watershed.        </dc:subject>
</item> 

 
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