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| Hauptseite > Publikationsdatenbank > Construction of Minirhizotron Facilities for Investigating Root Zone Processes > print |
| Hauptseite > Publikationsdatenbank > Construction of Minirhizotron Facilities for Investigating Root Zone Processes > print |
| 001 | 819510 | ||
| 005 | 20220930130107.0 | ||
| 024 | 7 | _ | |a 10.2136/vzj2016.05.0043 |2 doi |
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| 100 | 1 | _ | |a Cai, Gaochao |0 P:(DE-Juel1)156154 |b 0 |e Corresponding author |u fzj |
| 245 | _ | _ | |a Construction of Minirhizotron Facilities for Investigating Root Zone Processes |
| 260 | _ | _ | |a Madison, Wis. |c 2016 |b SSSA |
| 336 | 7 | _ | |a article |2 DRIVER |
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| 520 | _ | _ | |a Minimally invasive monitoring of root development and soil states (soil moisture, temperature) in undisturbed soils during a crop growing cycle is a challenging task. Minirhizotron (MR) tubes offer the possibility to view root development in situ with time. Two MR facilities were constructed in two different soils, stony vs. silty, to monitor root growth, root zone processes, and their dependence on soil water availability. To obtain a representative image of the root distribution, 7-m-long tubes were installed horizontally at 10-, 20-, 40-, 60-, 80-, and 120-cm depths. A homemade system was developed to install MR tubes in the silty soil in horizontally drilled straight holes. For the stony soil, the soil rhizotubes were installed in an excavated and subsequently backfilled pit. In both facilities, three subplots were established with different water treatments: rain sheltered, rainfed, and irrigated. To monitor soil moisture, water potential, and soil temperature, time domain reflectometer probes, tensiometers, and matrix water potential sensors were installed. Soil water content profiles in space and time were obtained between two MR tubes using cross-hole ground-penetrating radar along the tubes at different depths. Results from the first growing season of winter wheat (Triticum aestivum L.) after installation demonstrate that differences in root development, soil water, and temperature dynamics can be observed among the different soil types and water treatments. When combined with additional measurements of crop development and transpiration, these data provide key information that is essential to validate and parameterize root development and water uptake models in soil–vegetation–atmosphere transfer models. |
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| 700 | 1 | _ | |a Vanderborght, Jan |0 P:(DE-Juel1)129548 |b 1 |u fzj |
| 700 | 1 | _ | |a Klotzsche, Anja |0 P:(DE-Juel1)129483 |b 2 |u fzj |
| 700 | 1 | _ | |a van der Kruk, Jan |0 P:(DE-Juel1)129561 |b 3 |u fzj |
| 700 | 1 | _ | |a Neumann, Joschka |0 P:(DE-Juel1)145411 |b 4 |u fzj |
| 700 | 1 | _ | |a Hermes, Normen |0 P:(DE-Juel1)129470 |b 5 |u fzj |
| 700 | 1 | _ | |a Vereecken, Harry |0 P:(DE-Juel1)129549 |b 6 |u fzj |
| 773 | _ | _ | |a 10.2136/vzj2016.05.0043 |g Vol. 15, no. 9, p. 0 - |0 PERI:(DE-600)2088189-7 |n 9 |p |t Vadose zone journal |v 15 |y 2016 |x 1539-1663 |
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