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Root biomass and soil carbon distribution in hybrid poplar riparian buffers herbaceous riparian buffers and natural riparian woodlots on farmland

机译:农田杨树河岸缓冲带草本河岸缓冲带和天然河岸林地的根系生物量和土壤碳分布

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摘要

The objectives of this study were to compare coarse root (diameter > 2 mm) and fine root (diameter < 2 mm) biomass, as well as distribution of soil carbon stocks in 3 types of riparian land uses across 4 sites located in farmland of southern Québec, Canada: (1) hybrid poplar buffers (9th growing season); (2) herbaceous buffers; (3) natural woodlots (varying in tree species and age). For all land uses most of the root biomass was within the 0–20 cm depth range. Total coarse root biomass, to a 60 cm depth, ranged from 8.8-73.7 t/ha in woodlots, 0.6-1.3 t/ha in herbaceous buffers, and 9.2-27.3 t/ha in poplars. Total fine root biomass ranged from 2.68-8.64 t/ha in woodlots, 2.60-3.29 t/ha in herbaceous buffers, and 1.86-2.62 t/ha in poplars. Total root biomass was similar or higher in poplar buffers compared to a 27 year-old grey birch forest. This indicates that poplar buffers accelerated riparian soil colonisation by roots compared to natural secondary succession. Generally, fine root biomass in the surface soil (0–20 cm) was lower in poplar than in herbaceous buffers; the reverse was observed at greater depth. Highest coarse root biomass in the 40–60 cm depth range was observed in a poplar buffer, highlighting the deep rooted nature of poplars. On average, total soil C stocks (0–60 cm) were greater in woodlots than in riparian buffers. On most sites, soil C stocks tended to be lower in poplar buffers compared to adjacent herbaceous buffers, especially in surface soil, probably because of lower fine root biomass in poplar buffers. Across all sites and land uses, highest soil C stocks at the different soil depths were found in the soil layers of woodlots that also had the greatest fine root biomass. Strong positive linear relationships between fine root biomass and soil C stocks in the 0–20 cm depth range (R2 = 0.79, p < 0.001), and in the whole soil profile (0–60 cm) (R2 = 0.65, p < 0.01), highlight the central role of fine root biomass in maintaining or increasing soil C stocks.
机译:这项研究的目的是比较粗根(直径> 2 mm)和细根(直径<2mm)生物量,以及在南部农田的四个地点的三种河岸土地利用类型中土壤碳储量的分布加拿大魁北克:(1)杂种杨树缓冲液(第9个生长季节); (2)草本缓冲剂; (3)天然林地(树木种类和年龄不同)。对于所有土地利用而言,大多数根系生物量都在0-20厘米深度范围内。总粗根生物量达到60厘米深度,在林地中为8.8-73.7吨/公顷,在草木缓冲液中为0.6-1.3吨/公顷,在杨​​树中为9.2-27.3吨/公顷。在林地中,细根总生物量为2.68-8.64 t / ha,在草本缓冲液中为2.60-3.29 t / ha,在杨树中为1.86-2.62 t / ha。与27岁的白桦林相比,杨树缓冲液中的总根生物量相似或更高。这表明与自然次生演替相比,杨树缓冲液通过根部促进了河岸土壤定植。通常,杨树表层土壤(0-20 cm)中的细根生物量低于草本缓冲液;相反,观察到的深度更大。在杨树缓冲液中观察到40-60 cm深度范围内最高的粗根生物量,突显了杨树的深根特性。平均而言,林地中的土壤总碳储量(0-60 cm)比河岸缓冲带中的要多。在大多数地点,杨树缓冲液中的土壤碳储量往往比相邻的草本缓冲液要低,尤其是在表层土壤中,这可能是由于杨树缓冲液中的细根生物量较低。在所有场地和土地利用中,在不同土壤深度的最高土壤碳储量都在林地的土壤层中发现,这些土壤的细根生物量也最大。细根生物量与土壤碳库在0–20 cm深度范围内(R 2 = 0.79,p <–0.001)之间以及整个土壤剖面(0–60 cm)之间都具有强的正线性关系(R 2 = 0.65,p <0.01),突出了细根生物量在维持或增加土壤碳储量中的核心作用。

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