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首页> 外文期刊>International Journal of Plant & Soil Science >Laboratory Setup for Sensing Root-Induced Changes of Soil Hydraulic Properties in Soil Columns
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Laboratory Setup for Sensing Root-Induced Changes of Soil Hydraulic Properties in Soil Columns

机译:感应根引起土壤柱中土壤水力特性变化的实验室设置

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Structural porosity is a dynamic soil property with high spatio-temporal variability affected by many factors. In order to develop a quantitative understanding of root driven changes in soil hydraulic properties adequate measurement setups are required. A modular soil column setup for drainage experiments providing all data for inverse determination of soil hydraulic properties was developed. The aim of this paper is to present the overall setup, and to assess if the influence of an experimental factor (plant roots) can be captured by the system. The designed setup facilitates simultaneous measurements of soil water content (TDR-sensor), matric potential (tensiometer) and column bottom flux (balance) in 12 soil filled columns. In total 144 soil water sensors ensure a high spatial and temporal resolution (six 10?cm?layers per column, time steps?≥?5?min). An initial drainage experiment with 12 unplanted columns was combined with a second (final) drainage run investigating the variants mustard ( Sinapis alba L.), rye ( Secale cereale L.) and an unplanted control in four replicates. A specific data acquisition system was developed to operate the devices, and for data synchronization and management. The included semi-automatic trouble-shooting routine sustained long-term experiments. Our analyses showed very low inter-sensor variability for TDR-sensors and tensiometers (0.2???0.5% and 1.2???4%, respectively). Cumulative outflow data indicated only a minor contribution to variability (6.1%) between columns due to heterogeneity from filling. Therefore, a significant effect of the experimental factor plant root was not overlaid by higher variability due to undesired effects, and could be clearly identified. We concluded that the setup is adequate to identify root induced changes of soil hydraulic properties using designed experiments.
机译:结构孔隙度是一种动态土壤性质,受许多因素影响,时空变化很大。为了对土壤水力特性的根源驱动变化有定量的了解,需要足够的测量设置。开发了用于排水实验的模块化土壤柱设置,提供了用于反演土壤水力学特性的所有数据。本文的目的是介绍整体设置,并评估系统是否可以捕获实验因素(植物根系)的影响。设计的设置便于同时测量12根土壤填充柱中的土壤水分(TDR传感器),基质势(张力计)和柱底通量(平衡)。总共144个土壤水分传感器确保了较高的空间和时间分辨率(每列6个10?cm?层,时间步长≥?5?min)。最初的排水实验用12个未植入的色谱柱与第二个(最终)排水实验相结合,研究了芥末变种(Sinapis alba L.),黑麦(Secale graine L.)和未种植的对照,一式四份。开发了特定的数据采集系统来操作设备以及进行数据同步和管理。随附的半自动故障排除例程可进行长期的长期实验。我们的分析表明,TDR传感器和张力计的传感器间变异性非常低(分别为0.2%0.5%和1.2%4%)。累积流出数据表明,由于填充的异质性,仅对色谱柱之间的变异性有很小的贡献(6.1%)。因此,由于不希望的影响,实验因子植物根的显着效果不会被较高的变异性所覆盖,并且可以清楚地确定。我们得出的结论是,使用设计的实验,该设置足以识别根源引起的土壤水力特性变化。

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