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Cosmic Ray Neutron Probe: Uses, Calibration and Validation in Austria Soils Newsletter Vol. 38, No. 1, July 2015 Cosmic Ray Neutron Probe: Uses, Calibration and Validation in Austria A. Wahbi1, M. Vreugdenhil2, G. Weltin1, L. Heng1, M. Oismueller2, P. Strauss3 ,G. Dercon1 1Soil and Water Management & Crop Nutrition Subprogramme, Joint FAO/IAEA Division of Nuclear Techniques in Food and Agriculture, International Atomic Energy Agency (IAEA), Vienna, Austria 2Centre for Water Resource Systems, Vienna University of Technology (TU Vienna), Vienna, Austria 3Federal Agency for Water Management, Institute for Land & Water Management Research, Petzenkirchen, Austria The importance of surface soil water (rooting zone) has ranges from 268 to 323 m a.s.l. with a mean slope of 8%, become evident with climate change affecting rainfall the surface soil is light-coloured, coarse-textured, with patterns and crop production. The use of Cosmic Ray periodic water stagnation. Land use is mainly agriculture Neutron Probe (CRNP) for measuring surface soil water (87%) with small parcels of forest and pasture. The content has become increasingly popular. The advantage climate is humid with a mean annual air temperature of of CRNP is that it is a non-invasive technique for 9.3°C and annual rainfall of 716 mm. Temperature, measuring soil water content at an area-wide scale (600 rainfall and rainfall intensity have their peak in summer meter in diameter), providing an unprecedented scale of (Eder et al., 2010). An Iridium Global Satellite observation (Desilets and Zreda, 2013). It also, monitor Communications Network – antenna, mounted on top of soil water content integrated over the top 40 cm the CRNP, enables data transfer depending on the wetness of the soil equivalent to snow (http://cosmos.hwr.arizona.edu/Probes/StationDat/087/ind depth of about 20 cm. ex.php). Cosmic-ray neutrons are a by-product of chain reactions initiated at the upper atmosphere by primary cosmic rays. These particles collide with atmospheric gas molecules, unleashing cascades of secondary protons, neutrons and other subatomic particles, some of which penetrate down to sea level. Fast neutrons are generated by cascading particles (primarily cascade neutrons) throughout the atmosphere and in the upper few meters of Earth’s crust (Desilets and Zreda, 2014). For a wide range of soil characteristics, a “universal” shape-defining function can be used to convert neutron counting rates to soil water content for typical silica-dominated soils. This function is valid for neutrons in the epithermal to the faster flux of the spectrum (100-106 eV), where neutron absorption is minor. The N0 method is a site-specific calibration technique that depends mainly on the characteristics of the surroundings. The method is described as: 0808.0 ( *)115.0 (1) p N bd Figure. 1. The cosmic Ray Neutron probe (CRNP). 372.0 N0 An in-situ soil water network consisting of 31 stations of where θp is pore (or gravimetric) water content (g/g), ρbd 3 electromagnetic probes (Time domain Transmission; is dry soil bulk density (g/cm ), N is the corrected neutron TDT) measuring soil water contents at 4 depths (0.05, counts per hour (cph), N0 is an instrument specific 0.10, 0.20 and 0.50 m) over an area of 66 ha was calibrated parameter that represents the count rate over established (Vreugdenhil et al., 2013) to provide dry silica soils, and the values 0.0808, 0.372 and 0.115 continuous soil water data for analyzing soil water are derived from a semi-analytical solution of a neutron dynamics (Franz et al., 2013). In addition, soil water diffusion equation (Desilets et al., 2010). content in the upper 15 cm of the soil was measured using A CRNP (CRS 1000/B model) consisting of two neutron TDR probes during two field samplings in April 2014. counters (one tuned for slow, the other one for fast The pattern of sampling to estimate θp was decided such neutrons), data logger and an Iridium modem, has been that each sample location (and representative area) is installed at the Technical University Petzenkirchen given equal weight in the CRNP sensitivity. A total of 60 research station for Water Resource Systems, 100 km undisturbed samples were taken at 0-5, 5-10 and 15-20 west of Vienna (Figure 1). The elevation of the study area cm. and soil water content was determined. At the time of 9 Soils Newsletter Vol. 38, No. 1, July 2015 soil sampling, N was recorded (by CRNP) and N0 The preliminary results showed that the CRNP measured calculated from equation (1), which is used to calculate soil water contents reflecting rainfall pattern and snow soil water content. However, the N0 values have to be event (Figure 2). Further, this CRNP derived soil water tested from time to time to assure their stability at content is sensitive to the water content of the above different soil wetness and cropping conditions. Sixteen ground biomass (mismatched in June-September 2014, as stations of the TDT network (which are within the a results of the plant growth; Figure 2). The CRNP is also footprint of the CRNP) are used to validate the CRNP sensitive to snow cover, leading to a rise in measured data. surface soil water content, as in Feb-March 2014 Because no other instrument operates at a comparable comparison (Figure 2). scale, field validation is inherently difficult due to More field measurements are currently being carried out different agricultural practices. Therefore, comparing the using TDT, TDR and gravimetric technique to compare CRNP measurements with TDT measurements will with CRNP under different water contents and crop provide adequate validation of the CRNP. The preferred managements to identify the relationship between soil method is to compare the CRNP measurements with the water contents and N0 with an easy and reliable measure gravimetric water contents. This should be done at of plant water content to improve the reliability and different time and space. The drawback is that the performance of the CRNP. Better assessment of the independent measurements are then indirect, and their effective soil depth will also be an important component accuracy and bias have to be measured also. to solve. 60 40 Daily Rainfall (mm) 50 TDR 0-15 cm 35 Freezing indicator 40 CRNP readings (%) 30 TDT 0-20 30 Soil depth CRNP 25 (cm) 20 20 10 Soil depth CRNP(cm) Vl0 i 15 Figure 2. Validation of Cosmic Ray Neutron Probe at Petzenkirchen station (2013-14 seasons). References Eder, A., Strauss, P., Krueger, T., and Quinton, J.: Desilets, D. and M. Zreda, Footprint diameter for a Comparative calculation of suspended sediment loads cosmic-ray soil moisture probe: Theory and Monte with respect to hysteresis effects (in the Petzenkirchen Carlo simulations, Water Resources Research, 49 catchment, Austria), J. Hydrol., 389 (2010) 168-176. (2013) 3566-3575. Franz, T.E, M. Zreda, R. Rosolem and T.P.A. Ferre , A Desilets, D., and M. Zreda, Cosmic-ray hydrometrology: universal calibration function for determination of soil Measuring soil moisture with cosmic-ray neutrons, in moisture with cosmic-ray neutrons, Hydrology and E. Njoku, ed., Encyclopedia of Remote Sensing: Earth System Sciences, 17 (2013) 453-460, doi: Springer Reference, Berlin Heidelberg, Springer- 10.5194/hess-17-453-2013. Verlag (2014). Vreugdenhil, M., W. Dorigo, M. Broer, P. Haas, A. Eder, Desilets, D., M. Zreda, and T. P. A. Ferre, Nature’s P. Hogan, G. Blöschl, W. Wagner, Towards a high- neutron probe: Land surface hydrology at an elusive density soil moisture network for the validation of scale with cosmic rays, Water Resources Research., 46 SMAP in Petzenkirchen, Austria. Proceedings of (2010), W11505, doi:10.1029/2009WR008726. IGARSS 2013 (2013) 1865 - 1868 10 .
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