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81.
Michael R. Morris Brook O. Brouwer Jeremy K. Caves Mary J. Harner Jack A. Stanford 《Aquatic Sciences - Research Across Boundaries》2010,72(4):519-532
In floodplain primary succession, vegetation colonizes nitrogen-poor alluvial deposits and fertility improves as soil nitrogen
accumulates over time. It is generally assumed that vegetation assimilates the vast majority of its nitrogen from the soil;
however, recent studies have suggested that the hyporheic zone also may be an important nitrogen source. We investigated the
potential relative importance of hyporheic nitrogen by comparing fertility indices, specifically total (TN), dissolved inorganic
(DIN), potentially mineralizable (PMN) and ion exchange resin nitrogen (IERN) in both soils and the hyporheic zone at early,
mid and late succession stands on an expansive river flood plain. We also constructed mesocosms to assess growth of cottonwood
cuttings with access to soil and/or hyporheic water. We found TN and PMN increased from early to mid succession in both the
soil (to 10 cm) and hyporheic zone (in a 10 cm layer). While TN, DIN and PMN were an order of magnitude higher in the soil
than in the hyporheic zone, IERN was higher in the hyporheic zone, indicating that subsurface flow through the flood plain
may be important in delivering nitrogen to the root zone. However, even when flux was added to the hyporheic PMN pool, nitrogen
availability in the hyporheic zone (in a 10 cm layer) was vastly lower than soil PMN (to 10 cm). Further, the instantaneous
standing stock of DIN in the surface soil alone was about equal to the sum of the DIN pool, the mean subsurface flux and the
PMN pool in a 10 cm layer of hyporheic zone. In the mesocosm experiment, cottonwood cuttings with access to both soil and
hyporheic water grew fastest; however, they also had the lowest foliar nitrogen concentrations, indicating that this was not
due to greater nitrogen availability. In the field, nitrogen content of cottonwood foliage increased along with soil (but
potentially hyporheic as well) nitrogen accumulation during succession, suggesting the vegetation responded to increasing
nitrogen fertility. We conclude that at least on a per unit-volume basis, the hyporheic zone probably provides little nitrogen
relative to the surface soil, except on new alluvial bars that characteristically are nitrogen poor. Therefore, the hyporheic
zone is probably a much smaller nitrogen source for mature forests relative to the surface soil unless the vegetation exploits
a much larger volume of the hyporheic zone than surface soil. 相似文献
82.
Mary Finley-Brook 《The Professional geographer》2013,65(4):557-559
Books reviewed in this article: Kurt E. Engelmann and Vjeran Pavlakovic (eds.), Rural Development in Eurasia and the Middle East: Land Reform, Demographic Change, and Environmental Constraints Gregory C. Randall, America's Original GI Town: Park Forest, Illinois John B. Rehder, Delta Sugar: Louisiana's Vanishing Plantation Landscape Cathy D. Knepper, Greenbelt, Maryland: A Living Legacy of the New Deal Char Miller (ed.), Fluid Arguments: Five Centuries of Western Water Conflict Edward F. Bergman, The Spiritual Traveler: New York City: The Guide to Sacred Spaces and Peaceful Places Rachel Pain, Michael Barke, Duncan Fuller, Jamie Gough, Robert MacFarlane, and Graham Mowl, Introducing Social Geographies Tor A. Benjaminsen, and Christian Lund, (eds.), Politics, Property, and Production in the West African Sahel: Understanding Natural Resources Management Al Gedicks, Resource Rebels: Native Challenges to Mining and Oil Corporations Maryann P. Feldman and Nadine Massard (eds.), Institutions and Systems in the Geography of Innovation Richard Foglesong, Married to the Mouse: Walt Disney World and Orlando Annick Germain, and Damaris Rose, Montréal: The Quest for a Metropolis George F. Rengert, Mark T. Mattson, and Kristin D. Henderson, Campus Security: Situational Crime Prevention in High–Density Environments Vaclav Smil, Feeding the World: A Challenge for the Twenty–First Century Pu Miao (ed.), Public Places in Asia Pacific Cities: Current Issues and Strategies Lisa M. Benton and John Rennie Short (eds.), Environmental Discourse and Practice: A Reader Philip Scranton (ed.), The Second Wave: Southern Industrialization from the 1940s to the 1970s Barry Dalal–Clayton and David Dent, Knowledge of the Land: Land Resources Information and Its Use in Rural Development 相似文献
83.
84.
85.
Mark Lacy Mary Elizabeth Kaiser Gary J. Hill Steve Rawlings Gareth Leyshon 《Monthly notices of the Royal Astronomical Society》1999,308(4):1087-1095
Further imaging observations of a sample of radio sources in the North Ecliptic Cap are presented and a number of new identifications are made. Using redshifts from spectroscopic data presented in a companion paper by Lacy et al., the photometric properties of the galaxies in the sample are discussed. It is shown that: (1) out to at least z ≈0.6 radio galaxies are good standard candles irrespective of radio luminosity; (2) for 0.6≲ z ≲1 a large fraction of the sample has magnitudes and colours consistent with a non-evolving giant elliptical, and (3) at higher redshifts, where the R -band samples the rest-frame UV flux, most objects have less UV luminosity than expected if they form their stellar populations at a constant rate from a high redshift to z ∼1 in unobscured star-forming regions (assuming an Einstein–de Sitter cosmology). The consequences of these observations are briefly discussed. 相似文献
86.
Juraj Majzlan Peter Glasnák Robert A. Fisher Mary Anne White Michel B. Johnson Brian Woodfield Juliana Boerio-Goates 《Physics and Chemistry of Minerals》2010,37(9):635-651
Jarosite phases are common minerals in acidic, sulfate-rich environments. Here, we report heat capacities (C
p) and standard entropies (S°) for a number of jarosite samples. Most samples are close to the nominal composition AFe3(SO4)2(OH)6, where A = K, Na, Rb, and NH4. One of the samples has a significant number of defects on the Fe sites and is called the defect jarosite; others are referred
to as A-jarosite. The samples, their compositions, and the entropies at T = 298.15 K are:
There are additional configurational entropies of 13.14 and 8.23 J mol−1 K−1 in defect and NH4-jarosite, respectively. A detailed analysis of the synchrotron X-ray diffraction patterns showed a large anisotropic peak
broadening for defect and NH4-jarosite. The fits to the low-temperature (approx. <12 K) C
p data showed that our samples can be divided into two groups. The first group is populated by the K-, Na-, Rb-, and NH4-jarosite samples, antiferromagnetic at low temperatures. The second group contains the H3O-jarosite (studied previously) and the defect jarosite. H3O- and defect jarosite are spin glasses and their low-T
C
p was fit with the expression C
p = γT + ΣB
j
T
j
, where j = (3, 5, 7, 9). The linear term is typical for spin glasses and the sum represents the lattice contribution to C
p. Surprisingly, the C
p of the K-, Na-, Rb-, and NH4-jarosite samples, which are usually considered to be antiferromagnetic at low temperatures, also contains a large linear
term. This finding suggests that even these phases do not order completely, but have a partial spin-glass character below
their Néel transition temperature. 相似文献
Sample | Chemical composition | S o/(J mol−1 K−1) |
---|---|---|
K-jarosite | K0.92(H3O)0.08Fe2.97(SO4)2(OH)5.90(H2O)0.10 | 427.4 ± 0.7 |
Na-jarosite | Na0.95(H3O)0.05Fe3.00(SO4)2(OH)6.00 | 436.4 ± 4.4 |
Rb-jarosite | RbFe2.98(SO4)2(OH)5.95(H2O)0.05 | 411.9 ± 4.1 |
NH4-jarosite | (NH4)0.87(H3O)0.13Fe3.00(SO4)2(OH)6.00 | 447.2 ± 4.5 |
Defect jarosite | K0.94(H3O)0.06Fe2.34(SO4)2(OH)4.01(H2O)1.99 | 412.7 ± 4.1 |
87.
Long-term exposure of animals to sub-lethal doses of toxicants such as benzene (B) and dimethylnaphthalene (DMN) may result in subtle changes in their physiology and biochemistry. In crustaceans such changes include decreased rate of limb regeneration, extended time to molt and decreased growth increment at molt.1,2 These processes depend upon an adequate supply of stored nutrients in the tissues and appropriate release of neuroendocrine substances from the central nervous system.3,4 We are examining the effects of sub-lethal doses of B and DMN on osmotic and ionic regulation and on nutrient storage in the blue crab, Callinectes sapidus, and the green crab, Carcinus maenas. Disturbances in these physiological processes may reflect alterations in neuroendocrine functions brought about by the presence of toxicants. We find that exposure of C. maenas to B or DMN, followed by transfer to a dilute medium, results in impaired osmoregulatory capacity, while addition of these compounds to a dilute medium to which the animal is already acclimated does not affect their regulatory ability. Storage of carbohydrate in the midgut gland (hepatopancreas) is decreased by B or DMN, while the accessory storage tissues (gill, muscle) are not significantly affected. 相似文献
88.
Mary C. Bourke 《Icarus》2010,205(1):183-197
Barchan dune asymmetry refers to the extension of one barchan limb downwind. It is a common dune form on Earth and also occurs on Mars and Titan. A new classification of barchan limbs is presented where three types of limb morphology are identified: linear, kinked and beaded. These, along with other dune-scale morphological signatures, are used to identify three of the causes of barchan asymmetry on Mars: bi-directional winds, dune collision and the influence of inclined topography.The potential for specific dune asymmetric morphologies to indicate aspects of the formative wind regime on planetary surfaces is shown. For example, the placement of dune limbs can indicate the general direction and relative strength of formative oblique winds; an extreme barchan limb length may indicate a long duration oblique wind; a kinked limb may be evidence of the passage of a storm; beaded limbs may represent surface-wave instabilities caused by an increase in wind energy parallel to the dune. A preliminary application of these signatures finds evidence for bi-modal winds on Mars. However, these and other morphological signatures of wind direction and relative strength should be applied to planetary landforms with caution as more than one process (e.g., bi-modal winds and collision) may be operating together or sequentially on the dunefield. In addition, analysis should be undertaken at the dunefield scale and not on individual dunes. Finally, morphological data should be acquired from similar-scale dunes within a dunefield.In addition to bi-modal wind regimes on Mars, the frequent parallel alignment of the extended barchan limb to the dune suggests that dune collision is also an important cause of asymmetry on Mars. Some of the more complex dunefield patterns result from a combination of dune collision, limb extension and merging with downwind dunes.Dune asymmetric form does not inhibit dune migration in the Namib Desert or on Mars. Data from the Namib suggest that dune migration rates are similar for symmetric and asymmetric dunes. Further modeling and field studies are needed to refine our understanding of the potential range of limb and dune morphologies that can result from specific asymmetry causes. 相似文献
89.
In 2001, the National Oceanic and Atmospheric Administration (NOAA) and the Ministry of Maritime Affairs and Fisheries Integrated Coastal and Ocean Resources Scientific and Technical Arrangement was signed to pursue scientific and technical cooperation in integrated coastal and ocean resources management in the mutual interest of the participants. Over the last 6 years, the cooperation has been very beneficial, particularly for advancing marine science and management programs in Korea, such as Deep Sea Aquaculture, Sea Grant College Program, Marine Protected Areas, and Ocean Observations. The benefits to NOAA from the cooperation include Deep-ocean Assessment and Reporting of Tsunamis (DART) buoys, ocean and coastal observations, GEOSS program, and Global Program of Action. Also the cooperation has spillover effects on other ocean science and technological arrangement between US and Korea. This article reviews purpose, obstacles, and achievement of the cooperation and suggests recommendations for the future steps. 相似文献
90.
In this paper, we formulate a finite element procedure for approximating the coupled fluid and mechanics in Biot’s consolidation
model of poroelasticity. Here, we approximate the pressure by a mixed finite element method and the displacements by a Galerkin
method. Theoretical convergence error estimates are derived in a discrete-in-time setting. Of particular interest is the case
when the lowest-order Raviart–Thomas approximating space or cell-centered finite differences are used in the mixed formulation
and continuous piecewise linear approximations are used for displacements. This approach appears to be the one most frequently
applied to existing reservoir engineering simulators. 相似文献