Peter G. Cook

ORCID: 0000-0002-1418-8214
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About
Contact & Profiles
Research Areas
  • Groundwater flow and contamination studies
  • Groundwater and Isotope Geochemistry
  • Hydrology and Watershed Management Studies
  • Groundwater and Watershed Analysis
  • Hydraulic Fracturing and Reservoir Analysis
  • Soil and Unsaturated Flow
  • Geophysical and Geoelectrical Methods
  • Hydrocarbon exploration and reservoir analysis
  • Plant Water Relations and Carbon Dynamics
  • Hydrology and Sediment Transport Processes
  • Atmospheric and Environmental Gas Dynamics
  • Soil and Water Nutrient Dynamics
  • Reservoir Engineering and Simulation Methods
  • Geology and Paleoclimatology Research
  • Geophysical Methods and Applications
  • Mine drainage and remediation techniques
  • Soil erosion and sediment transport
  • Karst Systems and Hydrogeology
  • Flood Risk Assessment and Management
  • Radioactivity and Radon Measurements
  • Underwater Acoustics Research
  • Water Quality and Resources Studies
  • Cinema and Media Studies
  • Seismic Imaging and Inversion Techniques
  • Hydrological Forecasting Using AI

National Centre for Groundwater Research and Training
2015-2024

Flinders University
2015-2024

University of Pretoria
2020

Universidade Estadual Paulista (Unesp)
2020

University of Utah
2020

Aix-Marseille Université
2018-2019

University of South Australia
2018

Commonwealth Scientific and Industrial Research Organisation
2006-2015

CSIRO Land and Water
2006-2015

Imperial Oil (Canada)
2005

10.1007/s10040-001-0178-0 article EN Hydrogeology Journal 2002-01-12

Understanding how changes in the groundwater table affect surface water resources is of fundamental importance quantitative hydrology. If below a stream sufficiently deep, position effectively do not alter infiltration rate. This referred to as disconnected system. Previous authors noted that low‐conductivity layer body necessary but sufficient criterion for disconnection occur. We develop precise allows an assessment whether water–groundwater systems can disconnect or not. further...

10.1029/2008wr006953 article EN Water Resources Research 2009-01-01

Groundwater discharge to the Cockburn River, southeast Australia, has been estimated from comparison of natural 222 Rn activities in groundwater and river water, interpreted using a numerical flow model that simulates longitudinal radon as function inflow, hyporheic exchange, evaporation, gas exchange with atmosphere, radioactive decay. An injection SF 6 into estimate transfer velocity assisted constraining model. Previous estimates inflow have not considered possible input due between water...

10.1029/2006wr004921 article EN Water Resources Research 2006-10-01

Abstract Environmental tracer methods have been used to quantify groundwater discharge rivers for the past few decades. A number of different tracers in these studies, including individual ion concentrations, electrical conductivity, stable isotopes 2 H and 18 O, dissolved gases helium, chlorofluorocarbons radon. This paper discusses assumptions method, as well its resolution accuracy. The method will be most accurate when concentration is very distinct from that river. On basis typical...

10.1002/hyp.9493 article EN Hydrological Processes 2012-07-21

Chemical base flow separation is a widely applied technique in which contributions of groundwater and surface runoff to streamflow are estimated based on the chemical composition stream water two end‐members. This method relies assumption that end‐member can be accurately defined remains constant. We simulate solute transport within aquifer during after single multiple river events, show (1) adjacent will have concentration intermediate between regional (2) discharge approach event but may...

10.1029/2009wr008539 article EN Water Resources Research 2010-07-01

Abstract Traditionally, groundwater and surface water flow models have been calibrated against two observation types: hydraulic heads discharge. It has repeatedly demonstrated, however, that these classical observations do not contain sufficient information to calibrate models. To reduce the predictive uncertainty of models, consideration other types constitutes a promising way forward. Despite ever‐increasing availability types, they are still unconventional when it comes model calibration....

10.1029/2018rg000619 article EN Reviews of Geophysics 2019-02-20

Vast areas in the interior of Australia are exposed to regular but infrequent periods heavy rainfall, interspersed with long at high temperatures, little is known carbon budget these remote or how they respond extreme precipitation. In this study, we applied three methods partition net ecosystem photosynthesis into gross primary production (GPP) and respiration (R e ) during two years contrasting rainfall. The first year was wet (>250 mm above average rainfall), while precipitation fell...

10.1002/jgrg.20101 article EN Journal of Geophysical Research Biogeosciences 2013-07-01

Apparent ages obtained from the measured concentrations of environmental tracers have potential to inform recharge rates, flow and assist in calibration groundwater models. A number studies investigated sources error relationships between apparent ages, age assumed by models relate this quantity an aquifer property (e.g., recharge). These also provided a techniques for correcting known biases ages. In paper, we review some concepts bias. We then demonstrate bias through use on four numerical...

10.1111/gwat.12237 article EN Ground Water 2014-07-12

Abstract Intermittent rivers and ephemeral streams (IRES) account for over 50% of the world's river network are expected to increase with climate change increasing pressure on water resources. One significant challenge better manage IRES is unraveling threshold behavior streamflow generation, by understanding what controls triggers streamflow. This study aimed understand influence groundwater depth, soil hydraulic properties, rainfall generation in IRES, through analyzing spatiotemporal...

10.1029/2019wr025041 article EN publisher-specific-oa Water Resources Research 2019-10-23

Abstract Radium isotopes and radon are routinely used as tracers to quantify groundwater porewater fluxes into coastal freshwater systems. However, uncertainties associated with the determination of tracer flux often poorly addressed neglect all potential errors conceptualization system (i.e., conceptual uncertainties). In this study, we assess magnitude some key related radium inputs supplied by a waterbody (La Palme Lagoon, France). This uncertainty assessment is through single model...

10.1002/lno.11678 article EN Limnology and Oceanography 2021-01-08

Abstract Groundwater models that simulate only saturated flow use groundwater recharge as an input parameter. In contrast, variably subsurface models, including integrated surface and hydrologic can jointly the movement of water in unsaturated zones. Instead recharge, they require climate data such precipitation potential evapotranspiration. Given latter represent hydrological processes operating throughout zone at table, one might expect be readily extracted from them. this paper, we...

10.1029/2023wr034920 article EN cc-by-nc-nd Water Resources Research 2023-08-10

Driven by the need for integrated management of groundwater (GW) and surface water (SW), quantification GW–SW interactions associated contaminant transport has become increasingly important. This is due to their substantial impact on quantity quality. In this review, we provide an overview methods developed over past several decades investigate interactions. These include geophysical, hydrometric, tracer techniques, as well various modeling approaches. Different reveal valuable information...

10.1146/annurev-environ-111522-104534 article EN Annual Review of Environment and Resources 2024-07-18

Chlorofluorocarbons and krypton 85 are trace gases whose atmospheric concentrations have been increasing over the past few decades. As they soluble in water, used as groundwater age indicators timescales ranging from a years to In this paper we show that time lag for transport of these through unsaturated zone is an important consideration when dating groundwaters recharged thick zones. The apparent largely dependent on gas solubility, diffusion coefficient, soil water content....

10.1029/94wr02232 article EN Water Resources Research 1995-02-01

Detailed depth profiles of Chlorofluorocarbons CFC‐11(CFCl 3 (, CFC‐12 (CF 2 Cl ) and CFC‐113 (C F have been obtained from a well‐characterized field site in central Ontario. Aquifer materials comprise predominantly silty sands, with mean organic carbon content 0.03%. Nearly one‐dimensional flow exists at this site, the vertical migration well‐defined H peak has tracked through time. sampling allowed CFC tracer velocities to be estimated within 10%. Comparison enables estimation...

10.1029/94wr02528 article EN Water Resources Research 1995-03-01
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