Ian D. Moore

ORCID: 0000-0003-2446-1891
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About
Contact & Profiles
Research Areas
  • Geotechnical Engineering and Underground Structures
  • Geotechnical Engineering and Analysis
  • Geotechnical Engineering and Soil Stabilization
  • Structural Integrity and Reliability Analysis
  • Geophysical Methods and Applications
  • Hydrology and Watershed Management Studies
  • Soil erosion and sediment transport
  • Vibration and Dynamic Analysis
  • Seismic Imaging and Inversion Techniques
  • Geotechnical Engineering and Soil Mechanics
  • Mechanical stress and fatigue analysis
  • Soil and Unsaturated Flow
  • Seismic Waves and Analysis
  • Water Systems and Optimization
  • Concrete Corrosion and Durability
  • Underwater Acoustics Research
  • Advanced Fiber Optic Sensors
  • Drilling and Well Engineering
  • Dam Engineering and Safety
  • Engineering Structural Analysis Methods
  • Structural Load-Bearing Analysis
  • Asphalt Pavement Performance Evaluation
  • Soil and Water Nutrient Dynamics
  • Hydrology and Sediment Transport Processes
  • Rock Mechanics and Modeling

Queen's University
2016-2025

University of California, Santa Barbara
2025

Central Arkansas Veterans Healthcare System
2024

Royal Military College of Canada
2013-2023

Virginia Tech
2023

Schlumberger (British Virgin Islands)
2014-2019

Jacobs (United Kingdom)
2017

ACAL Energy (United Kingdom)
2017

Chevron (United States)
2016

Carleton University
2016

This study is based on the hypothesis that catenary soil development occurs in many landscapes response to way water moves through and over landscape. Furthermore, terrain attributes can characterize these flow paths and, therefore, attributes. Significant correlations between quantified measured were found a 5.4-ha toposequence Colorado. Slope wetness index most highly correlated with surface at 231 locations 15.24-m grid. Individually, they accounted for about one-half of variability A...

10.2136/sssaj1993.03615995005700020026x article EN Soil Science Society of America Journal 1993-03-01

Abstract The length‐slope factor in the universal soil loss equation (USLE) is a purely empirical relationship that was derived from an extensive data base. A physically based independently this paper by using unit stream power theory to describe erosion processes associated with sheet and rill flow on hill‐slopes. It shown two factors are equivalent. Therefore, USLE measure of sediment transport capacity runoff landscape, but fails fully account for hydrological affect erosion. strength...

10.2136/sssaj1986.03615995005000050042x article EN Soil Science Society of America Journal 1986-09-01

Abstract Explicit and quantitative models for the spatial prediction of soil landscape attributes are required environmental modelling management. In this study, advances in representation hydrological geomorphological processes using terrain analysis techniques integrated with development a field sampling soil-landscape model building strategy. Statistical developed relationships between (plan curvature, compound topographic index, upslope mean plan curvature) (A horizon depth, Solum E...

10.1080/02693799508902047 article EN International Journal of Geographical Information Systems 1995-07-01

Future directions for physically based, distributed‐parameter models intended use as hydrologic components of sediment and nutrient transport are discussed. The attraction these is their potential to provide information about the flow characteristics at points within catchments, but current representations in process‐based often too crude enable accurate, a priori application predictive problems. difficulties relate both perception model capabilities fundamental assumptions algorithms used...

10.1029/92wr01259 article EN Water Resources Research 1992-10-01

ABSTRACT THE relationship between topographic attributes and the distribution of surface soil water content in a small bare-fallow cultivated catchment was examined. The most statistically significant regression equations describing this contained independent variable aspect compound ln(A,), where A,=Ab/S A^ is local upslope contributing area per unit width contour line S slope. index measure saturation, product (A^.S), erosive power concentrated runoff, were both capable predicting location...

10.13031/2013.30829 article EN Transactions of the ASAE 1988-01-01

Theoretical equations for calculating the unit stream power of both sheet and rill flow were developed used to predict sediment transport capacity such flows. Independent data sets from three sources representing finely aggregated clay soils coarse textured nonaggregated soils, sheet, rill, composite systems, a range slopes test utility method. The results very good demonstrated simplicity robustness For shallow overland best obtained when critical at incipient motion was treated as constant...

10.1029/wr022i008p01350 article EN Water Resources Research 1986-08-01

THALES, a simple distributed parameter hydrologic model is presented and applied to two catchments in Australia the United States, each with different dominant responses. The simulates Hortonian overland flow runoff from saturated source areas used identify some of barriers modeling hydrology small catchments. At Wagga New South Wales, Australia, produced areas, whereas on Lucky Hills at Walnut Gulch Arizona, processes dominate. Simulations are based published parameters field data measured...

10.1029/92wr01258 article EN Water Resources Research 1992-10-01

An automated method of partitioning catchments into interconnected elements using a “stream tube” approach and vector or contour‐based digital elevation models is briefly described. With this form partitioning, hydrologic can be structured based on the hydraulics flow within catchment effects topography runoff producing mechanisms spatially distributed characteristics (such as depth velocity) directly, realistically, accounted for in models. The allows complex three‐dimensional problems to...

10.1029/91wr00090 article EN Water Resources Research 1991-06-01

A quasi‐dynamic wetness index that accounts for variable drainage times since a prior rainfall event is derived from simple subsurface flow theory. The method tested through series of field observations and numerical experiments using spatially distributed, dynamic hydrologic model. shown to be useful extension previously developed static indices predicting the location zones soil saturation distribution water (i.e., content overlying shallow impermeable or semiimpermeable layer). new not...

10.1029/93wr03346 article EN Water Resources Research 1994-04-01

Five mathematical models for predicting subsurface flow were compared to discharge measurements made by Hewlett and Hibbert (1963) on a uniform sloping soil trough at the Coweeta Hydrologic Laboratory. The included one‐ two‐dimensional finite element based Richards equation, kinematic wave model, two simple storage‐discharge Boussinesq assumptions. simulated response water table positions as well more complex equation much economical use from point of view computational costs. Such have...

10.1029/wr020i012p01815 article EN Water Resources Research 1984-12-01

A digital model for discretizing three-dimensional terrain into small irregularly shaped polygons or elements based on contour lines and their orthogonals is described. From this subdivision the estimates a number of topographic attributes each element including total upslope contributing area, slope, aspect. This form discretization catchment produces natural units problems involving water flow as either surface subsurface phenomenon. The therefore has wide potential application...

10.1002/esp.3290130404 article EN Earth Surface Processes and Landforms 1988-06-01

Abstract After dry summers or drought, eucalypt forest soils at two sites in southeastern Australia developed hydrophobic non‐wetting surface characteristics that reduced infiltration, measured using a sprinkling infiltrometer. At one site the development of conditions caused rainfall to runoff conversion efficiency forested catchment increase from 5 per cent 15 cent. Under non‐hydrophobic this site, grassland always generated more than forest. However, major rainfall‐runoff was recorded...

10.1002/hyp.3360030302 article EN Hydrological Processes 1989-07-01

Surface-related multiple elimination (SRME) is an algorithm that predicts all surface multiples by a convolutional process applied to seismic field data. Only minimal preprocessing required. Once predicted, the are removed from data adaptive subtraction. Unlike other methods of attenuation, SRME does not rely on assumptions or knowledge about subsurface, nor it use event properties discriminate between and primaries. In exchange for this “freedom subsurface,” requires acquisition wavelet...

10.1190/1.3475413 article EN Geophysics 2010-09-01

We describe a new algorithm that uses known firing times to separate data from two or more impulsive, simultaneous seismic sources. Synthetic and field tests show the works well, especially when are not spatially aliased. Aliasing effects can be reduced if assumptions, such as in some sense sparse, made.

10.1190/1.3063928 article EN 2008-01-01

Three-component measurements of particle motion would bring significant benefits to towed-marine seismic data if processed in conjunction with the pressure data. We show that velocity can increase effective Nyquist wavenumber by a factor two or three, depending on how they are used. A true multicomponent streamer enable accurate reconstruction crossline direction cable separations for which pressure-only be irrecoverably aliased. also conventional workflows aimed at reducing these aliasing...

10.1190/1.2953338 article EN Geophysics 2008-09-01

Seismic faulting is extremely detrimental to buried pipelines owing bending moments and axial forces generated by the soil–pipe interaction. Pipe responses ground rupture are usually evaluated beam-on-spring analysis. However, empirical data used define spring response were obtained for steel pipes with high flexural stiffness effectiveness of resulting values flexible questionable. This paper presents full-scale tests undertaken using a new split-box apparatus which permits testing in dry...

10.1680/jgeot.16.p.161 article EN Géotechnique 2017-05-08

Relative ground movement represents a severe seismic hazard to pipelines crossing faults, and the maximum expected pipeline strains are primary design concern. Past research has documented how stiff steel respond permanent deformation produced calibrated empirical models of response strike-slip normal faulting. However, what little data exist on flexible illustrate ‘stiff pipeline’ soil reaction significantly overestimate peak for pipelines. Results four centrifuge tests conducted model...

10.1680/jgeot.14.p.175 article EN Géotechnique 2015-12-16

Abstract Based on the experimental data presented in Part I, two uniaxial constitutive models are constructed. The first, a nonlinear viscoelastic (NVE) model, is formulated using mechanical analogy consisting of one independent spring and six Kelvin elements series. Creep used to determine model parameters. second viscoplastic (VP) formulation, developed theory proposed by Bodner characterize behavior metals. Inelastic strain rate introduced into state variable addition inelastic work...

10.1002/pen.11684 article EN Polymer Engineering and Science 1997-02-01

Abstract Cross sections of a 203‐mm diam. soil core taken from site under Kentucky bluegrass ( Poa pratensis L. ) were scanned using x‐ray computed tomography (CT) to determine if macropores such as cracks, earthworm holes and root channels could be distinguished characterized. The was physically sectioned at the same locations CT scans verify size location pores seen on images. Macropores 1 mm larger easily quickly by method. By manipulation scanner images, air‐filled pores, roots stones...

10.2136/sssaj1989.03615995005300030001x article EN Soil Science Society of America Journal 1989-05-01
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