Biomass, morphology and nutrient contents of fine roots in four Norway spruce stands
- 368 Downloads
Fine root systems may respond to soil chemical conditions, but contrasting results have been obtained from field studies in non-manipulated forests with distinct soil chemical properties. We investigated biomass, necromass, live/dead ratios, morphology and nutrient concentrations of fine roots (<2 mm) in four mature Norway spruce (Picea abies [L.] Karst.) stands of south-east Germany, encompassing variations in soil chemical properties and climate. All stands were established on acidic soils (pH (CaCl2) range 2.8–3.8 in the humus layer), two of the four stands had molar ratios in soil solution below 1 and one of the four stands had received a liming treatment 22 years before the study. Soil cores down to 40 cm mineral soil depth were taken in autumn and separated into four fractions: humus layer, 0–10 cm, 10–20 cm and 20–40 cm. We found no indications of negative effects of N availability on fine root properties despite large variations in inorganic N seepage fluxes (4–34 kg N ha−1 yr−1), suggesting that the variation in N deposition between 17 and 26 kg N ha−1 yr−1 does not affect the fine root system of Norway spruce. Fine root biomass was largest in the humus layer and increased with the amount of organic matter stored in the humus layer, indicating that the vertical pattern of fine roots is largely affected by the thickness of this horizon. Only two stands showed significant differences in fine root biomass of the mineral soil which can be explained by differences in soil chemical conditions. The stand with the lowest total biomass had the lowest Ca/Al ratio of 0.1 in seepage, however, Al, Ca, Mg and K concentrations of fine roots were not different among the stands. The Ca/Al ratio in seepage might be a less reliable stress parameter because another stand also had Ca/Al ratios in seepage far below the critical value of 1.0 without any signs of fine root damages. Large differences in the live/dead ratio were positively correlated with the Mn concentration of live fine roots from the mineral soil. This relationship was attributed to faster decay of dead fine roots because Mn is known as an essential element of lignin degrading enzymes. It is questionable if the live/dead ratio can be used as a vitality parameter of fine roots since both longevity of fine roots and decay of root litter may affect this parameter. Morphological properties were different in the humus layer of one stand that was limed in 1983, indicating that a single lime dose of 3–4 Mg ha−1 has a long-lasting effect on fine root architecture of Norway spruce. Almost no differences were found in morphological properties in the mineral soil among the stands, but vertical patterns were apparently different. Two stands with high base saturation in the subsoil showed a vertical decrease in specific root length and specific root tip density whereas the other two stands showed an opposite pattern or no effect. Our results suggest that proliferation of fine roots increased with decreasing base saturation in the subsoil of Norway spruce stands.
KeywordsCa/Al ratio Fine roots Fine root biomass Fine root morphology Liming Mn concentration Nitrogen deposition Norway spruce
We thank Rita Süss, Andreas Puhr, Sabine Horvarth, Kristin Strobel, and Regina Gerlinger for their assistance in the preparation of roots. We like to thank Stephan Raspe and Christoph Schulz from the Bayerische Landesanstalt für Wald und Forstwirtschaft and Wendelin Weis from the Technical University of Munich for providing element fluxes in throughfall and seepage of the four study sites. We are thankful to the members of the Central Analytical Laboratory of the Bayreuth Center of Ecology and Environmental Research (BayCEER) for chemical analysis of root samples. Financial support came from the Bavarian State Ministry of Agriculture and Forestry.
- Berg B, Ekbohm G, Johansson MB, McClaugherty C, Rutigliano F, Virzo De Santo A (1996) Some foliar litter types have a maximum limit for decomposition—a synthesis of data from forest systems. Can J Bot 74:659–672Google Scholar
- IUSS Working Group WRB 2006 World reference base for soil resources 2006. 2nd edn. World Soil Resources Report No. 103. FAO, RomeGoogle Scholar
- Joslin JD, Kelly JM, Wolfe MH (1988) Elemental patterns in roots and foliage of mature spruce across a gradient of soil aluminium. Water Air Soil Pollut 40:375–390Google Scholar
- Murach D, Schünemann E (1985) Reaktion der Feinwurzeln von Fichten auf Kalkungsmaßnahmen. AFZ 40:1151–1154Google Scholar
- Persson H, Von Fircks Y, Majdi H, Nilsson LO (1995) Root distribution on a Norway spruce (Picea abies (L.) Karst.) stand subjected to drought and ammonium-sulphate application. Plant Soil 168–169:1995Google Scholar
- Püttsepp U, Lõhmus K, Persson HA, Ahlstrom K (2006) Fine-root distribution and morphology in an acidic Norway spruce (Picea abies (L.) Karst.) stand in SW Sweden in relation to granulated wood ash application. For Ecol Manage 221:291–298Google Scholar
- Regent Instruments Inc (2003) WinRhizo 2003b, Basic, Reg & Pro For Washed Root MeasurementGoogle Scholar
- Rothe A (1997) Einfluß des Baumartenanteils auf Durchwurzelung, Wasserhaushalt, Stoffhaushalt und Zuwachsleistung eines Fichte-Buchen-Mischbestandes am Standort Höglwald. Forstl. Forschungsberichte München 163Google Scholar
- UBA (2006) Berichterstattung 2006 unter dem Übereinkommen über weiträumige grenzüberschreitende Luftverschmutzung (UN ECE-CLRTAP), http://www.umweltbundesamt.de/ emissionen/publikationen.htm