Subsidence hazards due to evaporite dissolution in the United States   总被引：1，自引：4，他引：1  

Kenneth S. Johnson 《Environmental Geology》2005,48(3):395-409

Evaporites, including gypsum (or anhydrite) and salt, are the most soluble of common rocks; they are dissolved readily to form the same type of karst features that typically are found in limestones and dolomites, and their dissolution can locally result in major subsidence structures. The four basic requirements for evaporite dissolution to occur are: (1) a deposit of gypsum or salt; (2) water, unsaturated with CaSO₄ or NaCl; (3) an outlet for escape of dissolving water; and (4) energy to cause water to flow through the system. Evaporites are present in 32 of the 48 contiguous states of the United States, and they underlie about 35–40% of the land area. Karst is known at least locally (and sometimes quite extensively) in almost all areas underlain by evaporites, and some of these karst features involve significant subsidence. The most widespread and pronounced examples of both gypsum and salt karst and subsidence are in the Permian basin of the southwestern United States, but many other areas also are significant. Human activities have caused some evaporite–subsidence development, primarily in salt deposits. Boreholes may enable (either intentionally or inadvertently) unsaturated water to flow through or against salt deposits, thus allowing development of small to large dissolution cavities. If the dissolution cavity is large enough and shallow enough, successive roof failures above the cavity can cause land subsidence or catastrophic collapse.  相似文献   

A dynamic programming model for optimal planning of aquifer storage and recovery facility operations   总被引：3，自引：0，他引：3  

V. Uddameri 《Environmental Geology》2007,51(6):953-962

Aquifer storage recovery (ASR) is an innovative technology with the potential to augment dwindling water resources in regions experiencing rapid growth and development. Planning and design of ASR systems requires quantifying how much water should be stored and appropriate times for storage and withdrawals within a planning period. A monthly scale planning model has been developed in this study to derive optimal (least cost) long-term policies for operating ASR systems and is solved using a recursive deterministic dynamic programming approach. The outputs of the model include annual costs of operation, the amount of water to be imported each month as well as the schedule for storage and extraction. A case study modeled after a proposed ASR system for Mustang Island and Padre Island service areas of the city of Corpus Christi is used to illustrate the utility of the developed model. The results indicate that for the assumed baseline demands, the ASR system is to be kept operational for a period of 4 months starting from May through August. Model sensitivity analysis indicated that increased seasonal shortages can be met using ASR with little additional costs. For the assumed cost structure, a 16% shortage increased the costs by 1.6%. However, the operation time of ASR increased from 4 to 8 months. The developed dynamic programming model is a useful tool to assess the feasibility of evaluating the use of ASR systems during regional-scale water resources planning endeavors.  相似文献   

Hurricane-induced landslide activity on an alluvial fan along Meadow Run, Shenandoah Valley, Virginia (eastern USA)     

Gerald F. Wieczorek  L. Scott Eaton  Thomas M. Yanosky  Eric J. Turner 《Landslides》2006,3(2):95-106

Although intense rainfall and localized flooding occurred as Hurricane Isabel tracked inland northwestardly across the Blue Ridge Mountains of central Virginia on September 18–19, 2003, few landslides occurred. However, the hurricane reactivated a dormant landslide along a bluff of an incised alluvial fan along Meadow Run on the western flanks of the Blue Ridge Mountains. Subsequent monitoring showed retrogressive movement involving several landslide blocks for the next several months. Using dendrochronology, aerial photography, and stream discharge records revealed periods of landslide activity. The annual variation of growth rings on trees within the landslide suggested previous slope instability in 1937, 1972, 1993, 1997, and 1999, which correlated with periods of local flood events. The avulsive and migrating nature of Meadow Run, combined with strong erosional force potential during flood stages, indicates that landslides are common along the bluff-channel bank interface, locally posing landslide hazards to relatively few structures within this farming region.  相似文献   

扫描式t检验的新应用:对美国西部近8000年干湿期的划分^*          下载免费PDF全文

谷湘潜  江剑民 《第四纪研究》2006,26(5):742-751

①中国气象科学研究院灾害天气国家重点实验室,北京 100081;②中国气象局培训中心,北京 100081; ③Joint Institute of Marine and Atmospheric Research, University of Hawaii, Honolulu, HI 96822 USA;④Pacific Fisheries Environmental Laboratory, NOAA/NMFS, Pacific Grove, CA 93950 USA)  相似文献   

Evaluating sedimentary geochemical lake-level tracers in Walker Lake, Nevada, over the last 200 years   总被引：1，自引：0，他引：1  

Fasong Yuan  Braddock K. Linsley  Stephen S. Howe 《Journal of Paleolimnology》2006,36(1):37-54

Walker Lake, a hydrologically closed, saline, alkaline lake located along the western margin of the Great Basin of western United States, has experienced a 77% reduction in volume and commitment drop in lake level as a result of anthropogenic perturbations and climatic fluctuations over the last century. The history of lake-level change in Walker Lake has been recorded instrumentally since 1860. A high-resolution multi-proxy sediment core record from Walker Lake has been generated through analysis of total inorganic carbon (TIC), total organic carbon (TOC), and oxygen and carbon isotope ratios (δ¹⁸O and δ¹³ C) of both downcore bulk TIC and ostracods over the last 200 yr. This allows us to examine how these sediment indices respond to actual changes in this lake’s hydrologic balance at interannual to decadal timescales. In Walker Lake sediments, changes in %TIC, %TOC, and δ¹³C and δ¹⁸O of TIC and ostracods are all associated to varying degrees with changes in the lake’s hydrologic balance, with δ¹⁸O of the TIC fraction (δ¹⁸O_TIC) being the most highly correlated and the most effective hydrologic indicator in this closed-basin lake. The δ¹⁸O_TIC record from Walker Lake nearly parallels the instrumental lake-level record back to 1860. However, comparison with sporadic lake-water δ¹⁸O and dissolved inorganic carbon δ¹³C (δ¹³C_DIC) results spanning the last several decades suggests that the isotopic values of downcore carbonate sediments may not be readily translated into absolute or even relative values of corresponding lake-water δ¹⁸O and δ¹³C_DIC. Changes in the lake’s hydrologic balance usually lead to changes in isotopic composition of lake waters and downcore sediments, but not all the variations in downcore isotopic composition are necessarily caused by hydrologic changes.  相似文献   

Dye dispersion in the surf zone: Measurements and simple models   总被引：1，自引：0，他引：1  

L.B. Clarke  D. Ackerman  J. Largier 《Continental Shelf Research》2007

To examine the spatial and temporal effect of low-volume land-based runoff on beach contamination, discrete batches of dye were released at the shoreline at three beaches in Santa Monica Bay in 2000 (Malibu Creek, Santa Monica Canyon and Pico–Kenter drain). Dye concentration was measured at the shoreline 25, 50 and 100 m alongshore from the dye release point for up to 40 min after dye release. The shoreline concentration time series are characterized either by approximately exponential decay in concentration after passage of the dye patch maximum concentration or by persistent low concentration up to 30 min after passage of the initial dye patch front. In the absence of detailed measurements of physical conditions, several simple advection–diffusion models are used to simulate shoreline concentration time series for an idealized surf zone in order to probe the roles of alongshore current shear and rip currents in producing the observed characteristics in dye concentration time series. Favorable qualitative and quantitative comparison of measured and simulated time series suggest alongshore current shear and rip currents play key roles in generating the observed characteristics of nearshore dye patch dispersion. The models demonstrate the potential effects of these flow features on the extent and duration of beach contamination owing to a continuous contamination source.  相似文献   

The Appearance of Ulva laetevirens（Ulvophyceae,Chlorophyta） in the Northeast Coast of the United States of America     

MAO Yunxiang  ;Jang Kyun Kim  ;Roderick Wilson  ;Charles Yarish 《青岛海洋大学学报(英文版)》2014,(5):865-870

Introduced species may outcompete or hybridize with native species, resulting in the loss of native biodiversity or even alteration of ecosystem processes. In this study, we reported an alien distromatic Ulva species, which was found in an embayment（Holly Pond） connected with Long Island Sound, USA. The morphological and anatomical observations in combination with molecular data were used for its identification to species. Anatomy of collected specimens showed that the cell shape in rhizoidal and basal regions was round and the marginal teeth along the basal and median region were not found. These characteristics were primarily identical to the diagnostic characteristics of Ulva laetevirens Areschoug（Chlorophyta）. The plastid-encoding tufA and nucleus-encoding ITS1 were used for its molecular identification. Phylogenetic analysis for the tufA gene placed the specimens from Holly Pond in a well-supported clade along with published sequences of U. laetevirens identified early without any sequence divergence. In ITS tree, the sample also formed well-supported clades with the sequences of U. laetevirens with an estimated sequence divergence among the taxa in these clades as low as 1%. These findings confirmed the morpho-anatomical conclusion. Native to Australia, this species was reported in several countries along the Mediterranean coast after the late of 1990 s. This is the first time that U. laetevirens is found in the northeast coast of United States and the second record for Atlantic North America.  相似文献   

美国海底地名标准化工作管窥     

刘连安  阮文斌  高钰 《广东海洋大学学报》2014,(5):42-49

美国是开展海底地名标准化工作较早的国家之一,以其全球视野开展海底地名工作,在国际上掌握了较大的话语权。通过在美国地名委员会内设立海底地名咨询委员会,对海底地名的命名原则、通名选用等方面进行明确规定,不断完善纪念性命名管理制度等,美国形成了比较严密的地名标准化管理和技术体系。这些对我国的海洋管理和地名标准化工作都有较高的参考价值。  相似文献   

Microbiological and chemical characterization of hydrothermal fluids at Tortugas Mountain Geothermal Area, southern New Mexico, USA   总被引：1，自引：1，他引：0  

Dirk Schulze-Makuch  John F. Kennedy 《Hydrogeology Journal》2000,8(3):295-309

The Tortugas Mountain Geothermal Area is part of the larger hydrothermal system of the Rio Grande Rift, southern New Mexico, USA. Chemical and microbial parameters indicate that the sampled hydrothermal water derives from a mixture zone of deep, anaerobic water with meteoric water from an adjacent alluvial, non-thermal groundwater flow system. A microbial phospholipid fatty acid (PLFA) analysis indicates that biomass and diversity of hydrothermal groundwater are very low, whereas hydrothermal surface water is diverse and bacteria are in a rapid growth phase. A nucleic acid (DNA) analysis of the hydrothermal groundwater resulted in the identification of one eubacterium and two Archaea (archaebacteria); the eubacterium and one Archaea were previously unknown. The one Archaea that could be related to a known species is an extreme halophilic methanomicrobacterium. The presence of the halophilic Archaea and the other Archaea species supports the hypothesis of the Tortugas Mountain Geothermal Area being the discharge area of deep circulating groundwater within a bedrock-hosted regional groundwater flow system. Received, April 1999/Revised, January 2000/Accepted, February 2000  相似文献   

A groundwater-basin approach to conceptualize and simulate post-Pleistocene subsurface flow in a semi-arid region, southeastern New Mexico and western Texas, USA     

Thomas F. Corbet 《Hydrogeology Journal》2000,8(3):310-327

Numerical simulation was used to enhance conceptual understanding of the post-Pleistocene hydrogeology of a layered sequence of clastic and evaporite sediments. This work is part of an effort to evaluate the suitability of the Waste Isolation Pilot Plant (WIPP), New Mexico, USA, as a repository for transuranic waste. The numerical model is three-dimensional, extends laterally to topographic features that form the actual boundaries of a regional groundwater system, and uses a free surface with seepage face as an upper boundary condition to simulate the effect of change in recharge rate on the position of the water table. Simulation results suggest that the modern-day flow field is still adjusting to the drying of the climate that has occurred since the end of the Pleistocene Epoch. A wetter climate at the end of the Pleistocene resulted in a shallow water table, and patterns of groundwater flow were controlled by the intermediate features of the land-surface topography. As the climate became drier and the water table declined, groundwater flow began to increasingly reflect the land-surface topography at the scale of the entire groundwater basin. The modern-day flow pattern has not equilibrated with either the present recharge rate or the position of the water table. Received, November 1998/Revised, December 1999/Accepted, January 2000  相似文献