Estimation of bottom scattering strength from measured and modeledmid-frequency sonar reverberation levels

Hamilton-type geoacoustic models were developed for Area Foxtrot, a shallow water test bed south of Long Island, for emerging active sonar systems where the surface sediment type is highly spatially variable. Reverberation levels (RL) were modeled using the finite-element parabolic equation (FEPE) propagation model to augment the generic sonar model (GSM) propagation model because the bottom loss model in GSM did not estimate transmission loss (TL) accurately in shallow water. FEPE estimates reveal that there is a greater than 15 dB difference between TL for sand and that for silt-day sediments in Area Foxtrot. The comparison between modeled RL and measured RL (from a 1991 active sonar exercise) enabled bottom scattering strength kernels to be developed for Area Foxtrot. Bottom scattering strength was found to be a function of sediment type. Hard sand sediment has a bottom scattering strength which obeys Lambert's law (sin² &thetas;) while that of silt-clay sediment is consistent with sub-bottom volume scattering (sine). The RLs in Area Foxtrot are azimuth-dependent and are a function of TL and bottom scattering strength (and hence bottom sediment type). Sonar beams steered towards the hard sand show higher RLs than for silt-clay, and knowledge of the sediment type and its spatial variation must be known to model RL accurately. A method to determine sediment type using measured RLs and RL slopes is given     

13C‐rich marbles from the Proterozoic Einasleigh metamorphics,northern Queensland

Four samples of dolomitic marble from the Proterozoic Einasleigh Metamorphics of northern Queensland contain unusually high δ¹³C (5.1 to 5.9‰ PDB). A hyper‐saline depositional and diagenetic environment for these rocks adequately explains the available field and chemical evidence, and the heavy carbon signature.     

Second-Hand Spaces: Restructuring Retail Geographies in an Era of E-Commerce

Are online markets replacing or remaking second-hand markets in cities? The restructuring of secondary markets in light of virtual outlets like eBay is not well understood. In this article, we describe secondary markets and their important historic, economic, cultural, and social roles in cities. The literature on e-Commerce suggests that virtual retailers compete with bricks-and-mortar stores and potentially displace them. We question whether the internet can substitute for second-hand stores, which have traditionally relied on a loyal and local customer base, personalized shopping experiences, and surprise encounters. Given the historically embedded nature of exchange, we focus on one large Mid-western city, drawing upon survey and interview data from Chicago retailers. Our exploration of supply, demand, and geographic practices reveals subtle and complex alterations in second-hand exchange, rather than a displacement of second-hand markets by eBay. We also find substantive integration, fluidity, and hybridization within and across market sectors. Rather than supplant the production of new goods, secondary markets are intertwined with and deepen primary markets, calling into question some of the presumed benefits of and meanings associated with second-hand exchange as well as the usefulness of categorical distinctions. [Key words: secondary markets, second-hand, resale, thrift, e-commerce, eBay.]     

Critical GIS pedagogies beyond ‘Week 10: Ethics’

Over two decades after the scholarly interventions that coalesced into ‘critical GIS’ as a field within GIScience, critical GIS remains underdeveloped in conversations on teaching and learning. The literature on GIScience education has emphasized content more than pedagogies – what to teach versus how to teach to move students toward particular learning objectives. This emphasis is reflected in dominant curricular approaches to critical GIS, in which questions around the complicated origins and complicit social, political, and economic relationships of GIS are taken up as discrete topics, tacked onto instruction that otherwise prioritizes technical dimensions of GIScience. We argue that GIScience coursework must resist such modularization by approaching critical GIS not as a set of topics, but an orientation to GIS praxis that ‘does’ GIS from within a questioning stance, to ask how we know. We outline specific curricular shifts and teaching practices we have used to foster this orientation in GIS students, offering ways of continually engaging students in practicing this orientation as they learn strong technical GIScience content. Finally, we trace the successes, challenges, and tensions sparked by these critical GIS pedagogies, drawing on student evaluation comments from our courses and reflecting on broader implications for GIScience instructors and geography faculty.     

Water requirements for germination and early seedling establishment in four African savanna woody plant species

The aim of this study was to determine the water requirements for germination and early seedling establishment of four African savanna tree species, namelyAcacia karroo, A. nilotica, A. tortilisandMundulea sericea. The acacias are characteristic of nutrient-rich, andM. sericeaof nutrient-poor savannas. Imbibition times of scarified seeds ofA. karroo(4 h),M. sericea(6 h) andA. tortilis(8 h) were rapid relative toA. nilotica(28 h) and were inversely correlated with seed size. Imbibed water is lost in about 2 h after drying at 25°C for all species exceptA. nilotica(only 70% moisture loss). Seeds ofA. karrooandM. sericeakept at 40°C dried to below their original moisture contents within 2 h. Seeds ofA. niloticaandA. tortilisdried at 40°C lost viability relative to (undried) control seeds, while there was no significant loss of viability forA. karrooandM. sericea. For fully imbibed seeds to germinate in sandy savanna soils, all four species required at least the equivalent of 3 mm rainfall every 2 days under mild greenhouse conditions. However, most ungerminated seeds were still viable despite drying-out from a fully imbibed state. Maintenance of soil at 50% field capacity (FC), or watering to FC every 9th day is the maintenance requirements for 2-week-old seedlings ofA. niloticaandM. sericeato continue growth for a further 5 weeks under greenhouse conditions, althoughA. niloticamostly survived 25% FC with one seedling surviving 12·5% FC. Root penetration was rapid in sandy soils, withA. niloticaandM. sericeaattaining a depth of 40 cm within 15 days. Frequent, but not necessarily high, rainfall appears to be essential for germination and seedling survival over the first 7 weeks.     

Econometric and learning curve estimation of U.S. potential oil supply

This study employs (1) a simple econometric model to generate a time series of drilling footage to the year 2040 and (2) learning models to estimate the oil reserve additions from that drilling, given scenarios of oil price and projected U.S. population. Reserve additions are estimated separately for the lower 48 states and Alaska regions by estimating separate drilling footage and learning models for each region. Generally, the estimates of potential supply from undiscovered oil fields and from extensions of known fields are more optimistic than recent estimates by others. For a $1989 price of about $20/barrel (bbl), which is similar to recent prices, the potential supply of oil is estimated to be approximately 60.7 billion bbl, with 95-percent confidence bounds of 54.3 and 67.1 billion bbl. For a price of $25.50/bbl, potential supply is estimated to be approximately 82 billion bbl, with 95-percent confidence bounds of 74.5 and 89.5 billion bbl. Although estimates of potential oil supply for the entire United States are more optimistic than other recent estimates, the part of that supply estimated to be forthcoming from Alaska is smaller than other recent estimates: 2.3 and 3.3 billion bbl for prices of about $20 and $25.50 per barrel, respectively. Thus, reserve additions from the lower 48 states through development drilling and through improved recovery and production technologies will become increasingly important to future U.S. oil supply.     

The influence of<Emphasis Type="Italic">Phragmites</Emphasis> (common reed) on the distribution,abundance, and potential prey of a resident marsh fish in the Hackensack Meadowlands,New Jersey

This study investigates the influence ofPhragmites australis (common reed) invasion on the habitat of the resident marsh fish,Fundulus heteroclitus (mummichog) in the Hackensack Meadowlands, New Jersey. These abundant fish play an important role in the transfer of energy from the marsh surface to adjacent subtidal waters and thus estuarine food webs. The objectives of this 2-yr study (1999 and 2000) were to compare the distribution and abundance of the eggs, larvae, juveniles, and adults of mummichog and their invertebrate prey inhabitingSpartina alterniflora-dominated marshes withPhragmites-dominated marshes, and to experimentally investigate the influence of marsh surface microtoprography on larval fish abundance withinPhragmites-dominated marshes. In 2000, we verified that egg deposition does occur inPhragmites-dominated marshes. In both years, the abundance of larvae and small juveniles (4–20 mm TL) inS. alterniflora was significantly greater than inPhragmites-dominated marshes, while larger juveniles and adults (>20 mm TL) were similarly abundant in both habitat types. The overall abundance of larvae and small juveniles was significantly greater in experimentalPhragmites plots in which microtopography was manipulated to resemble that ofSpartina marshes than inPhragmites control plots. Major groups of invertebrate taxa differed between marsh types with potential prey for larval fish being significantly more abundant inS. alterniflora marshes.Phragmites-dominated marshes may not provide the most suitable habitat for the early life-history stages of the mummichog. The low abundance of larvae and small juveniles inPhragmites marshes is likely due to inadequate larval habitat and perhaps decreased prey availability for these early life history stages.