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ARS Home » Midwest Area » St. Paul, Minnesota » Soil and Water Management Research » Research » Publications at this Location » Publication #141444


item Baker, John

Submitted to: Agronomy Journal
Publication Type: Peer Reviewed Journal
Publication Acceptance Date: 1/20/2003
Publication Date: 6/23/2003
Citation: Baker, J.M. 2003. Recalcitrant problems in environmental instrumentation. Agronomy Journal. 95:1404-1407.

Interpretive Summary: All fields of science are bounded by measurement limitations, but it is not always clear which areas are most in need of further development. This review summarizes the most critical measurement needs in the area of environmental physics. Four major areas have been identified: 1) exchange processes between surface and atmosphere; 2) water and solute movement through soil; 3) measurement of the water status of plants; and 4) measurement of the nutrient content of soils and plants. The problems that limit our measurement abilities in each of these areas are described, as are the prospects for future improvements. The information should be useful to young scientists who are planning their research programs.

Technical Abstract: Frontiers in any science are generally defined by measurement limitations, and that is especially true in environmental iophysics. Among the more persistent issues are surface/atmosphere exchange, soil water and solute fluxes, plant water status, and plant/soil nutrient status. Measurement of surface/atmosphere exchange is particularly critical to global climate change research. Despite advances in instrumentation, accuracy of flux measurements, particularly eddy covariance, remains unacceptable, partly because the underlying assumptions of stationarity and surface homogeneity are so restrictive. Even when these assumptions are valid, the method appears to systematically underestimate, for reasons that are not yet well understood. Similarly, soil water and solute fluxes cannot yet be measured accurately and routinely, hampering water quality research. Recent advances in tension lysimetry offer hope for improvement, but most field experiments still rely on modeling of water and solute flow, supported by indirect measurements of ancillary variables, e.g. - soil water content, soil water otential, and solute concentration at discrete points in time and space. A third area of ongoing concern is that of plant water status. The major uncertainty here concerns which property should be measured. Nearly all of the effort over the past thirty years has been directed at measuring water potential, but water potential measurements are equilibrium measurements, and plants operate in dynamic environments. Furthermore, many physiological processes appear to be more related to relative water content than to water potential. Finally, more accurate and more timely (e.g. in situ) measurements of plant/soil nutrient status are sorely needed to take advantage of the promise of precision agriculture.