Impacts of snow-farming on alpine soil and vegetation: A case study from the Swiss Alps

被引:4
作者
Buttler, Alexandre [1 ,2 ]
Teuscher, Roland [3 ]
Deschamps, Nicolas [1 ]
Gavazov, Konstantin [2 ]
Bragazza, Luca [4 ]
Mariotte, Pierre [1 ,2 ]
Schlaepfer, Rodolphe [1 ]
Jassey, Vincent E. J. [1 ,2 ,5 ]
Freund, Lucas [1 ,4 ]
Cuartero, Jessica [6 ]
Quezada, Juan Carlos [1 ,4 ,7 ,8 ]
Frey, Beat [6 ]
机构
[1] Ecole Polytech Fed Lausanne EPFL, Sch Architecture Civil & Environm Engn ENAC, Stn 2, CH-1015 Lausanne, Switzerland
[2] Swiss Fed Inst Forest Snow & Landscape Res WSL, Site Lausanne, Stn 2, CH-1015 Lausanne, Switzerland
[3] Ob Bahnhofstr 22, CH-3714 Frutigen, Switzerland
[4] Agroscope, Field Crop Syst & Plant Nutr, Route Duillier 50,POB 1012, CH-1260 Nyon, Switzerland
[5] Agroscope, Grazing Syst Grp, CH-1725 Posieux, Switzerland
[6] Univ Paul Sabatier, CNRS, Lab Ecol Fonct & Environm, F-31062 Toulouse, France
[7] Swiss Fed Inst Forest Snow & Landscape Res WSL, CH-8903 Birmensdorf, Switzerland
[8] Nanyang Technol Univ, Asian Sch Environm, 50 Nanyang Ave, Singapore 639798, Singapore
基金
瑞士国家科学基金会;
关键词
Ski resort; Snow pile; Carbon; Nitrogen; Anaerobic microorganism; Saprotrophic microorganism; Alpine pasture; Biodiversity; NITROGEN MINERALIZATION; ANAEROBIC BACTERIUM; MICROBIAL ACTIVITY; EXTRACTION METHOD; SEED BANK; SKI RUN; SP NOV; BIOMASS; GRASSLAND; RESPIRATION;
D O I
10.1016/j.scitotenv.2023.166225
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Snow-farming is one of the adaptive strategies used to face the snow deficit in ski resorts. We studied the impact of a shifting snow-farming technique on a pasture slope in Adelboden, Switzerland. Specifically, we compared plots covered by a compressed snow pile for 1.5, 2.5 or 3.5 years, which then recovered from the snow cover for three, two or one vegetation seasons, respectively, with control plots situated around the snow pile. In plots with > 1.5 years of compressed snow pile, plant mortality was high, recovery of vegetation was very slow, and few plant species recolonized the bare surface. Soil biological activity decreased persistently under prolonged snow cover, as indicated by reduced soil respiration. The prolonged absence of fresh plant litter and root exudates led to carbon (C) limitation for soil microbial respiration, which resulted in a significant decrease in the ratio of total organic carbon to total nitrogen (TOC/TN) under the snow pile. Microbial C, nitrogen (N) and phosphorus (P) immobilization decreased, while dissolved N concentration increased with compressed snow cover. Longer snow cover and a subsequent shorter recovery period led to higher microbial C/P and N/P but lower microbial C/N. Nitrate and ammonium were released massively once the biological activity resumed after snow clearance and soil aeration. The soil microbial community composition persistently shifted towards oxygen-limited microbes with prolonged compressed snow cover. This shift reflected declines in the abundance of sensitive microorganisms, such as plant-associated symbionts, due to plant mortality or root die-off. In parallel, resistant taxa that benefit from environmental changes increased, including facultative anaerobic bacteria (Bacteroidota, Chloroflexota), obligate anaerobes (Euryarchaeota), and saprophytic plant degraders. We recommend keeping snow piles in the same spot year after year to minimize the area of the impacted soil surface and plan from the beginning soil and ecosystem restoration measures.
引用
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页数:15
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