By James F. Hogan, Fred M. Phillips, Bridget R. Scanlon
Released by way of the yankee Geophysical Union as a part of the Water technological know-how and alertness Series.
Groundwater recharge, the flux of water around the water desk, is arguably the main tough section of the hydrologic cycle to degree. In arid and semiarid areas the matter is exacerbated by way of super small recharge fluxes which are hugely variable in area and time.
--from the Preface
Groundwater Recharge in a wasteland surroundings: The Southwestern United States speaks to those matters via providing new interpretations and learn after greater than 20 years of discipline-wide examine. Discussions ondeveloping environmental tracers to fingerprint assets and quantities of groundwater on the basin scalethe severe position of plants in hydroecological processesnew geophysical tools in quantifying channel rechargeapplying Geographical info approach (GIS) versions to land floor processescoupling process-based vadose region to groundwater modeling, and extra make this e-book an important source for hydmlogists, biogeoscientists, and geochemists concerned about water and water-related concerns in arid and semiarid regions.
Read Online or Download Groundwater Recharge in a Desert Environment: The Southwestern United States PDF
Best geophysics books
The aim of utilized Geothermics for Petroleum Engineers is to give in a transparent and concise shape equipment of using the information of temperature surveys in deep boreholes in addition to the result of box, laboratory and analytical investigations in geothermics to a large viewers. even though a few points of the topic of this booklet were mentioned in different prior books and various papers, utilized Geothermics for Petroleum Engineers is the 1st booklet in this subject on hand to the petroleum engineering neighborhood.
Concerning the ProductPublished by way of the yank Geophysical Union as a part of the Antarctic study sequence. content material:
Concerning the ProductPublished via the yankee Geophysical Union as a part of the AGU Reference Shelf sequence. the aim of this guide is to supply, in hugely available shape, chosen severe info for pro and pupil stable Earth and planetary geophysicists. assurance of themes and authors have been conscientiously selected to meet those pursuits.
- Riparian Vegetation and Fluvial Geomorphology
- Seismic Reflection Processing: With Special Reference to Anisotropy
- Tectonic Inheritance in Continental Rifts and Passive Margins
- An Introduction to Applied and Environmental Geophysics
- Selected Papers from Volumes 26 and 27 of Vychislitel'naya Seysmologiya
- Collisionless Shocks in the Heliosphere: A Tutorial Review
Additional resources for Groundwater Recharge in a Desert Environment: The Southwestern United States
Bristow,Equationfor extending water-retentioncurvesto dryness,Soil Sci. Am. , 55,923927, 1991. , andJ. R. ,30, 701-708, 1994. Scanlon,B. , Evaluation of moistureflux from chloride data in desertsoils,J. , 128,137-156, 1991. Scanlon,B. , Moistureandsoluteflux alongpreferredpathways characterizedby fissuredsedimentsin desertsoils,J. Contam. , 10, 19-46, 1992. Scanlon,B. , Water and heat fluxes in desertsoils 1. Res. 30, 709-719, 1994. Scanlon,B. , andP. C. D. Milly, Water andheatfluxesin desert soils 2.
The authorsgratefully acknowledge helpfulcommentsprovidedby anonymousreviewers. Vol. 9 AND SCANLON 27 in Estimationof Natural GroundwaterRecharge,editedby I. Simmers,pp. 49-72, D. , 1988. Andraski, B. , 33, 1901-1916, 1997. Betancourt,J. , T. R. S. 'TheLast 40,000 Yearsof Biotic Change,The Univ. of Ariz. , 1990. Brooks,R. , and A. T. , FortCollins,1964. , R. B. Jackson,and J. R. Ehleringer,Maximum rooting depthof vegetationtypesat the global scale,Oecologia, 108, 583-595, 1996. , G. S. Campbell,andT.
The field lay dormant from 1983 through1991, goingback into production in the springof 1992. Since1992, irrigationratesin field 2 have been about the same as in field 1. Field 3 went into productionshortlyafter field 2. Until the early 1970'sthe field producedturf. The field producedalfalfa starting in 1987. 8 m per year. Irrigationwater is pumpedfrom individualwells (one for eachfield). The field-1 well was sampledin February2001. The field-2 well was sampledin January2002. The field-3 well was sampled in March 1974, February 2001, and Vol.