Bitterlich Michael, Franken Philipp, Graefe Jan
Leibniz Institute of Vegetable and Ornamental Crops, Großbeeren, Germany.
The Department of Plant Physiology, Humboldt University of Berlin, Berlin, Germany.
Front Plant Sci. 2018 Mar 7;9:301. doi: 10.3389/fpls.2018.00301. eCollection 2018.
Arbuscular mycorrhizal fungi (AMF) proliferate in soils and are known to affect soil structure. Although their contribution to structure is extensively investigated, the consequences of those processes for soil water extractability and transport has, so far, gained surprisingly little attention. Therefore we asked, whether AMF can affect water retention and unsaturated hydraulic conductivity under exclusion of root ingrowth, in order to minimize plant driven effects. We carried out experiments with tomato inoculated with in a soil substrate with sand and vermiculite that created variation in colonization by mixed pots with wild type (WT) plants and mycorrhiza resistant (RMC) mutants. Sampling cores were introduced and used to assess substrate moisture retention dynamics and modeling of substrate water retention and hydraulic conductivity. AMF reduced the saturated water content and total porosity, but maintained air filled porosity in soil spheres that excluded root ingrowth. The water content between field capacity and the permanent wilting point (6-1500 kPa) was only reduced in mycorrhizal substrates that contained at least one RMC mutant. Plant available water contents correlated positively with soil protein contents. Soil protein contents were highest in pots that possessed the strongest hyphal colonization, but not significantly affected. Substrate conductivity increased up to 50% in colonized substrates in the physiologically important water potential range between 6 and 10 kPa. The improvements in hydraulic conductivity are restricted to substrates where at least one WT plant was available for the fungus, indicating a necessity of a functional symbiosis for this effect. We conclude that functional mycorrhiza alleviates the resistance to water movement through the substrate in substrate areas outside of the root zone.
丛枝菌根真菌(AMF)在土壤中大量繁殖,并且已知会影响土壤结构。尽管对它们对土壤结构的贡献进行了广泛研究,但迄今为止,这些过程对土壤水分可提取性和运输的影响却惊人地受到很少关注。因此,我们提出疑问,在排除根系生长的情况下,AMF是否会影响持水性和非饱和导水率,以便将植物驱动的影响降至最低。我们在含有沙子和蛭石的土壤基质中对接种了AMF的番茄进行了实验,通过与野生型(WT)植物和抗菌根(RMC)突变体的混合盆栽创造了定殖差异。引入采样芯并用于评估基质持水动力学以及对基质持水性和导水率进行建模。AMF降低了饱和含水量和总孔隙度,但在排除根系生长的土壤球体中保持了通气孔隙度。只有在含有至少一个RMC突变体的菌根基质中,田间持水量和永久萎蔫点(6 - 1500 kPa)之间的含水量才会降低。植物有效含水量与土壤蛋白质含量呈正相关。在菌丝定殖最强的花盆中土壤蛋白质含量最高,但未受到显著影响。在6至10 kPa的生理重要水势范围内,定殖基质中的基质导水率提高了50%。导水率的提高仅限于至少有一株WT植物可供真菌利用的基质,这表明这种效应需要功能性共生。我们得出结论,功能性菌根减轻了根区以外基质区域中水分通过基质移动的阻力。