Spatial distribution of fine-roots in boreal forests in eastern Sweden

Investigations were carried out in six forest types in areas surrounding two Swedish nuclear power plants (Forsmark and Laxemar). The aim of the investigation was to determine the spatial distribution of fine-root biomass (live), necromass (dead) and standing crop (live + dead) and to test the use of the live/dead ratio as a vitality criterion. Soil cores were taken to depths with insignificant amounts of roots. The total amount of fine-root biomass (<1 mm in diameter) of tree species in the soil profile was 267, 317 and 235 g m^?2 for the Forsmark and 137, 371 and 50 g m^?2 for the Laxemar sites. The related necromass was 119, 226 and 184 g m^?2 and 87, 245 and 271 g m^?2. The biomass in the humus layer was 47, 7 and 48% for the Forsmark and 34, 26 and 7% for the Laxemar sites, as a percentage of the total live + dead fine roots in the soil profile. The related necromass in the humus layer was 13, 2 and 30% for the Forsmark and 13, 2 and 28% for the Laxemar sites. The live/dead ratio decreased with depth for both tree— and field-layer species and seems to be a most powerful vitality criterion of fine roots.     

Nitrogen supply and the control of expansive growth and function in leaves and roots

In plants which have acclimatized to limiting supplies of nitrogen (steady-state nutrition), leaf expansion (numbers and sizes of leaves and cells) is under tight control. Over a wide range of nitrogen supplies, the control of leaf growth is associated with a narrow band of photosynthetic rate per leaf area (measured at the growth climate) and, at limiting supplies, a carbon uptake which is in excess of immediate carbon usage in structural growth.For every increment of nitrogen absorbed, root extension is greater at limited nitrate supply, but V_max values (per root dry weight) for nitrate absorption are typically less. However, the capacity of the whole root system for nitrate uptake at limited supply is sufficient to allow for maximum growth, should nitrate supply be increased.It is concluded that a better understanding at the cellular level of the mechanisms which result in a greater inhibition of the expansion of single leaves than of root extension would contribute to an understanding of differences in carbon sink strength among plant organs. This may be a crucial step towards a more physiologically-based appreciation of plant dry matter distribution among organs in plants experiencing different nitrogen supplies.     

Fine root dynamics in a Norway spruce forest (Picea abies (L.) Karst) in eastern Sweden

The annual dynamics of live and dead fine roots for trees and the field layer species and live/dead ratios were investigated at a coniferous fern forest (Picea abies L. Karts) in Sweden. Our methods of estimating the average amount of fine roots involved the periodic sampling of fine roots in sequential cores on four sampling occasions. The highest live/dead ratio was found in the upper part of the humus layer for both tree and field-layer species and decreased with depth. Most tree fine roots on the four sampling occasions were found in the mineral soil horizon, where 86, 81, 85 and 89% of <1 mm and 89, 88, 89 and 92% of <2 mm diameter of the total amounts of live fine roots in the soil profile were found. The mean amounts of live fine roots of tree species for the total soil profile on the four sampling occasions was 317, 150, 139 and 248 g m^?2 for <1 mm and 410, 225, 224 and 351 g m^?2 for <2 mm diameter fine roots. The related amount of dead fine roots was 226, 321, 176 and 299 g m^?2 and 294, 424, 282 and 381 g m^?2, respectively. Average amounts of live and dead fine-roots and live/dead ratios from other Picea abies forest ecosystems were within the range of our estimates. The production of fine roots, <1 and <2 mm in diameter, estimated from the annual increments in live fine roots, was 207 and 303 g m^?2. The related accumulation of dead fine roots was 257 and 345 g m^?2, The turnover rate of tree fine roots <1 mm in diameter in the total soil profile amounted to 0.7 yr^?1 for live and 0.8 yr^?1 for dead fine roots. The related turnover rates for tree fine roots <2 mm were 0.4 yr^?1 and 0.7 yr^?1. Our data, although based on minimum estimates of the annual fluxes of live and dead fine roots, suggests a carbon flow to the forest soil from dead fine-roots even more substantial than from the needle litter fall. Fine-root data from several Picea abies forest ecosystems, suggest high turnover rates of both live and dead tree fine-roots.