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Quantifying Recreation Use Values From Removing Dams And

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[29] The bottom of Table 3 also illustrates the calculation of present value (PV) and average annual equivalent value (AAEV) of recreation benefits over the 100 year time period of analysis at the USACOE discount rate of 6.875%. The annual benefits grow from $185 million to $403 million over the 20 year time period, with an annualized value of

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Water And Sanitation Service Delivery, Pricing, And The

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Capital costsc c Ten percent real discount rate; 30 year average useful life of capital. 1.10: Wastewater serviceb b Cost estimates assume 35% nonrevenue water. 1.46: Operations and maintenance: 0.30: Capital costsc c Ten percent real discount rate; …

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Observations, Meteorites, And Models: A Preflight

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Thermal inertias are the highest for asteroids smaller than about 10 km, with values between about 200 and 800 J m −2 s −1/2 K −1. All cited thermal inertias are here normalized to the temperature conditions experienced at 1 AU, see Delbo et al. . For larger asteroids, values range typically from just under 10 to about 300 J m −2 s −1

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Linking Climate Projections To Performance: A Yield‐based

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It has been argued that such an approach would enable planners to either discount the need for GCMs in cases where the system performance is found to be poorly linked to climate variables, or tailor specific decision-critical thresholds to fit with the available climate information [Brown and Baroang, 2011; Brown and Wilby, 2012].

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Constraints On Cooling Of The Lower Ocean Crust From

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We discount the possibility that the epidote veins recorded cooling within the first 0.1 Myr (i.e., within 5- to 7-km off axis) and hence were witnesses of vigorous near-axial hydrothermal circulation that efficiently cooled the crystallizing lower crust (Figure 9a). First, the Sr (and O) isotopic compositions (set by water-rock ratios, i.e

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Robust Earthquake Early Warning At A Fraction Of The Cost

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For greater San Jose as well as Costa Rica's coastal regions, 10% expected peak ground acceleration (PGA) exceedance over the next 50 years is 0.55–0.90 g, in the upper ranges of global seismic hazard (Pagani et al., 2020).

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Louisville Seamount Chain: Petrogenetic Processes And

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1 Introduction. The Louisville Seamount Chain (LSC) is a 4300 km long chain of seamounts and guyots [Lonsdale, 1988] in the South Pacific, extending from 139°10′W, 50°26′S, in the vicinity of the Heezen Fracture Zone, to the Tonga-Kermadec Trench (175°18′W, 25°42′S; Figure 1).Menard et al.[] first reported the existence of an 1100 km long section of the chain

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The Primacy Of Doubt: Evolution Of Numerical Weather

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The evolution of numerical weather forecasting, from its formulation as a scientific initial value problem at the beginning of the 20th century, to today's complex numerical models has been described in the accurately titled review: “The quiet revolution of numerical weather prediction” [Bauer et al., 2015].Here it is shown how the skill of deterministic “best-guess” weather forecasts

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The Costs Of Coping With Poor Water Supply In Rural Kenya

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Median total coping costs per month are approximately US$20 per month, higher than average household water bills in many utilities in the United States, or 12% of reported monthly cash income. We estimate that coping costs are greater than 10% of income for over half of …

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Quantifying The Magnitude Of Anomalous Solar Absorption

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The CM22 and TSBR values differ by 5–10 W m −2, with the TSBR being greater on one day and the CM22 on the other. If we use the aircraft albedo values, which are each lower than the 10-m-tower value , the absorption decreases by 10 W m −2 on 27 February and 5 W m −2 on 20 March.

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Multiobjective Optimization Of Urban Water Resources

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A 5% discount rate was used. While Figure 3 displays a substantial cost trade-off between scenarios 3 and 4, the analysis of Figures 4 and 5 suggests that it is not straightforward to interpret the difference in solutions. The interactions between decisions appear to involve, in many cases, more than two variables. The color code

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Roughness Of Fault Surfaces Over Nine Decades Of Length

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1. Introduction [2] Faults appear most commonly as more or less continuous linear breaks at the surface of the Earth, and their traces show wavy irregularities at all scales [Brown and Scholz, 1985].These irregularities, which we call roughness, control the geometry [Power et al., 1987], mechanics, and transport properties of fault zones [Power and Durham, 1997] and contribute to their …

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Comparing Drinking Water Treatment Costs To Source Water

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The ECM allows for the examination of long-run relationships for source water quality and costs to better understand the conditions when water quality and cost variables move together [Greene, 1993].Because DWTPs often adjust treatment processes to accommodate episodic events (e.g., rainfall/runoff-induced excess turbidity), it also affords insight to short-run deviations from the long run …

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Multiobjective Optimization Of Cluster‐scale Urban Water

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For this study, a discount rate of 6% per annum was chosen for the economic objective. This is an intermediate value from among the range used by government agencies. For example, discount rates used among U.S., English, and Dutch government agencies range from 2 to 10% per annum [ Rambaud and Torrecillas , 2005 ] and South Australia's water

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Household Demand For Water In Sweden With Implications Of

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amount of water. The mean of the maximum discounts given by these communities is 0.70 Swedish Kronor (SEK) m -3 in 1980 prices (1 SEK - $0.15 (U.S. dollars) on average 1980- 1992), i.e., on average a 12% maximum discount on the total price. About 10% of Swedish communities use different

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Incorporating Multidimensional Probabilistic Information

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Economic discount rate (EDR) From 2% to 10%: explore the impacts on the decision of many plausible PDFs of many relevant classes of future conditions and trade them off against each other in a posterior sensitivity analysis. BNDS offers flexibility to respond to one of the most fundamental precepts of deep uncertainty, that informed

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Regime‐shifting Streamflow Processes: Implications For

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A failure period is defined as a period for which the lowest release class (10% of R D) cannot be delivered due to insufficient water in the reservoir plus incoming inflows Q t. Whilst supply failure implies high penalty cost, the two performance metrics offer different views of performance, since penalty costs can be incurred by over

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Distribution Of Seismicity Across Strike‐slip Faults In

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To assess the effects of earthquake clustering, we declustered the fault segment catalogs using the algorithm of Reasenberg with default parameters (r fact = 10, x k = 0.5, x meff = 1.5, τ 0 = 2 days, τ max = 10 days, p 1 = 0.99) and obtained the distribution parameters …

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Wild 2 And Interstellar Sample Collection And Earth Return

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If one assumes a 25% intact recovery for cometary grains, a 15 μm impacting particle would result in a 10 μm collected particle. On the basis of the modeled dust fluxes from Wild 2, a 1039 cm 2 collector area would be sufficient sweep up more than 1000 analyzable 10 μm particles, as indicated by the rightward arrow in Table 1.

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Model Development For Integrated Assessment Of Water

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The limit to off-allocation extraction is determined using commence to pump and cease to pump rules agreed to by the Namoi Regulated River Management Committee [DLWC, 1998]. These rules state: [44] 1. Maximum total annual off-allocation diversion of water in the regulated system is 110 GL. [45] 2. If available water for irrigation (ɛ) exceeds

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Episodicity In Phytoplankton Dynamics In A Coastal Region

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Virtual particles are seeded evenly in the domain at 24 h intervals and allowed to advect for 7 days using the off-line Lagrangian particle code TRACMASS. Satellite data are attached to the particle each time it intersects with a coincident observation (Figure 2). This matchup is done by pairing each cell on the model grid with the nearest

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Origin Of Earth's Water: Chondritic Inheritance Plus

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Based on the molar abundance ~1.82 × 10 −5 of Ne in Earth's atmosphere, which has a mass of 5.15 × 10 18 kg, this distribution implies that 1.1 × 10 14 moles of 22 Ne were ingassed. Likewise, the inferred abundance of 22 Ne in the deep mantle is 1.9 × 10 −14 mol/g (Yokochi & Marty, 2004 ) which, if considered as an average primitive

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Hydrologic Controls And Anthropogenic Drivers Of The Zebra

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The symbol (†) indicates parameter values that are not estimated via numerical fitting. The weights used to evaluate the aggregated objective function J for each of the three models are w i = 2.3 × 10 −5, w ii = 4.5 × 10 −6 and w iii = 0.15, as resulting from the …

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Imaging Crustal And Upper Mantle Structure Beneath The

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The consistent pipe-like upper mantle structures discount the possibility of an artifact introduced by an incorrect crustal thickness constraint. The shallow Moho inversion is preferred in this study because the data from the top positive event in the RF analysis is more physically reasonable since it is above 50 km.

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Multiobjective Design Of Water Distribution Systems Under

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[10] To solve the above system of nonlinear equations, all heads at tanks and reservoirs and statuses of time controlled pumps and valves must be specified as boundary conditions. The above system of equations can then be solved using a number of different methodologies. Here, the Epanet2 hydraulic solver [Rossman, 2000], based on the gradient algorithm introduced by Todini and Pilati is …

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A Multiple‐realizations Chance‐constrained Model For

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High nutrient loads in surface waters are a cause of hypoxia in coastal ecosystems. Constructed wetlands offer a means of nutrient removal, but their design is complicated by environmental fluctuatio

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Comparing Price And Nonprice Approaches To Urban Water

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The literature contains only a handful of industrial elasticity estimates. The results of five studies, 1969–1992, are reported by Griffin, ranging from −0.15 for some two-digit SIC codes [Renzetti, 1992a], to −0.98 for the chemical manufacturing industry [Ziegler and Bell, 1984].

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Classification Of Sea Ice Summer Melt Features In High

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1 Introduction. The 40-year satellite-derived record of Arctic sea ice extent reveals a negative and accelerating trend (−12.8% per decade) in the month of September at the sea ice minimum (Comiso et al., 2008; Richter-Menge et al., 2019).This decrease in summer ice extent has resulted in an increase in solar radiation absorption in the Arctic, spurring further ice melt through a positive

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Model Development For Integrated Assessment Of Water

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The limit to off‐allocation extraction is determined using commence to pump and cease to pump rules agreed to by the Namoi Regulated River Management Committee [DLWC, 1998]. These rules state: [44] 1. Maximum total annual off‐allocation diversion of water in the regulated system is 110 GL. [45] 2. If available water for irrigation (ɛ

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Mineralogical Controls On Frictional Strength, Stability

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The μ value defines the propensity for failure, while (a‐b) values define the mode of slip, as stable, aseismically (i.e., a‐b > 0), or unstable, seismically (i.e., a‐b < 0; Kohli & Zoback, 2013; Samuelson & Spiers, 2012).. Abundant experimental studies have revealed the values of frictional strength and frictional stability of a variety of rock materials, such as shales, tuffs

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Water‐rich And Volatile‐undersaturated Magmas At Hekla

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This signal had a source at 5.6 km depth, with an estimated volume of 5 × 10 6 −6 × 10 6 m 3. Geirsson et al . [ 2012 ] used GPS data to model a horizontal ellipsoid magma chamber at a depth of 24 ± 4 km depth, a spherical magma chamber at 24 ± 5 km depth, or a vertical pipe‐shaped chamber stretching between 10 and 21 km.

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Diagnosis Of Insidious Data Disasters

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1 Introduction. Measurements and modeling have gone hand‐in‐hand since before hydrology began as a formal science. In most early work [e.g., Mulvany, 1851; United States Army Corps of Engineers (US ACE), 1956], the same person took the measurements and developed the model, and iterated between them until all information collectively made sense.. The principal challenges of …

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Ground‐Based Optical Measurements Of Quiet Time

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The wind correction for this case is ∼10 m/s, which is statistically significant. However, unlike the wind correction, the temperature correction can be independently verified by observations. In this section we present direct observational evidence of the effect of atmospheric scattering on ground-based temperature measurements.

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Framework To Evaluate The Worth Of Hydraulic Conductivity

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Optimal total groundwater production varied between 8.69 × 10 3 m 3 /d and 10.37 × 10 3 m 3 /d, with an average production of 9.66 × 10 3 m 3 /d and a standard deviation of 0.25 × 10 3 m 3 /d. Thus the effect on the optimal solution of considering different realizations, as expressed by the relative magnitude of the standard deviation, was

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Water And Carbon Cycles In The Mississippi River Basin

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With the current CO 2 concentration of 360 ppm, the atmosphere contains 63.6 × 10 15 moles of CO 2 [Schlesinger, 1997]. The quantity of photosynthetically available water in the soils (i.e., root zone) is about 3228 to 3600 × 10 15 moles [Webb et al., 1993; Berner and Berner, 1996].

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Seismic Tomography Of Shatsky Rise By Adaptive Importance

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We thus applied a pressure correction of 0.2 × 10 −3 km s −1 MPa −1 and a temperature correction of −0.4 × 10 −3 km s −1 °C −1 [Korenaga et al., 2002], using a linear conductive geotherm with a thermal gradient of 11°C km −1 and a surface temperature of 0°C, which is appropriate for ∼140 Ma old oceanic lithosphere.

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Cost Of Water For Peace And The Environment In Israel: An

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Access to the posted model code in GAMS is described in Appendix Appendix A. 4 Results 4.1 Price and Use. Table 1 shows results of the optimized price and use of water by year, peace treaty obligation, environmental flow requirements, cost of desalination, and type of water use. It shows outcomes for 24 combinations of time periods (2), treaty

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Determination Of The Volcanostratigraphy Of Oceanic Crust

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By analogy with observations of the modern EPR [Macdonald et al., 1996] and the need for significant topography to pond such a thickness of lava, this massive flow is interpreted to have solidified 5 to 10 km off axis [Wilson et al., 2003].

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Dynamic Response Of Oceanic Hydrate Deposits To Ocean

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For k = 10 −14 m 2, the system exhibits no significant increase in Q Aq compared to the base case II (k 0 = 10 −15 m 2) up to t = 11 years, followed by a dramatic change in both the time of arrival of gas (Δt = −20 years) and the magnitude of Q G, which peaks at Q G = 0.28 m 3 /a STP, or 12.5 mol/a per m 2 of seafloor.

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In Search Of An Ice Core Signal To Differentiate Between

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[24] Ethane (C 2 H 6), ethene (C 2 H 4) and propane (C 3 H 8) show substantially different sensitivities in Sink 1 and Source 1, decreasing by 50–60% and 10–15%, respectively. Furthermore, these percentage changes equate to nonnegligible changes in concentration, of between 1 and 10 pptv.

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Rates And Mechanisms Of Turbulent Dissipation And Mixing

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Typically, 10%–30% of this energy is found to dissipate within 1 km of the seabed. Comparison between turbulent dissipation rates inferred from finestructure parameterizations and microstructure-derived estimates suggests a significant departure from wave-wave interaction physics in the near-field of wave generation sites.

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Formal And Informal Decision Making On Water Management At

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A village accommodates the farmers of the downstream plots of one to three nearby secondary canals. A growing number of plot holders are however outsiders to the village. In the rehabilitated parts of the irrigation scheme, outsiders comprise some 10 to 40% of plot holders [Jamin and Doucet, 1994]. In addition, even though illegal, leasing out

40

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A Technology‐based Global Inventory Of Black And Organic

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For most combustion-generated carbonaceous particles, PM 2.5 is 10 to 15% higher than PM 1.0 [e.g., Durbin et al., 1999a]. Inventories of BC and OC in the PM 2.5 range might be 10 to 15% higher than the values presented here. Cooke et al. estimated global “bulk” BC and OC emissions as 25% and 40% higher than submicron particles

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Wind‐wave‐induced Velocity In ATI SAR Ocean Surface

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The color code is the same as in Figure 1 with bright colors representing the data for the aft‐looking antenna pair and pale colors representing data for the fore‐looking antenna pair. The blue curve in (right) represents the projected component of the sea surface current as measured by the ADCP (westward ebb flow) at every azimuth angle.

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Fuzzy Probabilistic Design Of Water Distribution Networks

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Comparing to the fuzzy random formulation, these solutions lie at the bottom end of the Pareto fronts of cases H1 and H2 and have a very low reliability. The fuzzy random method provides a range of highly reliable solutions for the decision maker who is willing to trade off increased cost for improved system reliability. 4.2.3. Discussion

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Modeling Integrated Water User Decisions In Intermittent

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Calibration found the percentages of vacant and partially occupied connections as 10% and 15%, respectively. [52] The K-S Test ( D statistic = 0.019; n 1 = 20; n 2 = 500) indicates that the distributions of billed and modeled piped water use are similar at the 98% significance level ( Figure 3 ).

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Along‐strike Growth Of The Ostler Fault, New Zealand

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Oscillations of climate at ∼10 4-yr time scales modulate the formation and incision of geomorphic surfaces during successive glacial stages. Superimposed on apparently steadier rates of fault slip, such climate-dependent surfaces contribute to a pattern of progressive drainage deflection along the central Ostler fault zone that is largely

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Sr‐Nd‐Pb‐Hf Isotope Results From ODP Leg 187: Evidence For

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Sites 1152 and 1163 are located in what is the off‐axis equivalent of Zone B4 today. Sites 1155, 1156, and 1164 are located in Zone B5. All other sites are located in Zone A. Sites 1153, 1157, 1158, 1161, and 1162 form a N‐S transect <150 km east of the province‐bounding fracture zone at 127°E; we will refer to these as being located in

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How Paleosols Influence Groundwater Flow And Arsenic

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1. Introduction [2] In the Bengal Basin, the health of domestic consumers of groundwater has been adversely affected by arsenic pollution [Dhar et al., 1997; Smith et al., 2000; Saha and Chakraborti, 2001; Chakraborti et al., 2003; Ravenscroft et al., 2009].Although the distribution of arsenic pollution in wells is known spatially, from studies in both West Bengal [Public Health Engineering

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