Potential influence of landscape transition on stream water chemistry trends during the last decades in a karst catchment (Pyrenees, SW France) in a context of global environmental changes

Ecological Indicators

E. Vrech¹  A. Probst²  J.L. Probst²  C. Marais-Sicre³  F. Ulloa-Cedamanos⁴  E. Maire⁴ 

[1] Corresponding authors at: Laboratoire Ecologie fonctionnelle et Environnement, Université de Toulouse, CNRS, 31326 Castanet Tolosan, France.;LTER Bassin versant du Baget, SNO Karst, IR OZCAR, CNRS, University of Toulouse, France;LTSER Zone Atelier Pyrénées-Garonne, CNRS, University of Toulouse, France;Laboratoire Ecologie fonctionnelle et Environnement, Université de Toulouse, CNRS, 31326 Castanet Tolosan, France;

关键词: Landscape indicator;    Hydrochemical indicator;    Chemical weathering;    Long-term trends;    Climate change;    Acid deposition;   

DOI  :  

来源: DOAJ

【 摘 要 】

Over the last century, lands used for livestock and agriculture have been progressively abandoned on mountains across Europe. The afforestation of abandoned agricultural lands leads to significant environmental impacts particularly in karst catchments, which are highly responsive to climate change and human disturbances. Due to the lack of long-term historical records and appropriate methods, these impacts are not yet well investigated. The remote Baget forested catchment (Pyrenees Mountains), where a long-term hydrochemical survey has been conducted since 1979, was chosen to develop a method for reconstructing the evolution of landscapes based on heterogeneous and multi-temporal satellite imagery and aerial photographs from 1942 onwards. An indicator of landscape change is proposed, based on three vegetation groups, compatible with the various supporting data. The spatio-temporal landscape evolution evidenced a regular increase of 31% in forest extension between 1942 and 2019, while pioneer (grassland and heathlands) and open forest (early woodland) stages showed an overall but uneven decrease, marked by an accelerated decline of the latter due to an increase in livestock activities. The trends of streamwater discharge and chemistry were related to these environmental changes. A set of processes influencing the changes in the hydrochemical patterns, particularly the increase in dissolved elements in streamwater originating from carbonate dissolution, is proposed and discussed. The forest recolonization (+0.05 Km2.yr−1) enhanced soil organic matter content, generating an increased pCO2 in soils, which in turn enhanced the carbonate dissolution, expressed by a concentration increase of + 5 μeq.L-1.yr−1 for (Ca2++Mg2+) and of + 10 μeq.L-1.yr−1 for HCO3–. The steeper slope of HCO3– could result from decreasing terrestrial Ca2++Mg2+ export together with decreasing SO42- leaching (−4 μeq.L-1.yr−1) due to decreasing acid atmospheric deposition. In the meantime, the observed increase in air temperature (+0.03 °C.yr−1) favoured tree growth, litter decomposition and water demand by trees. This study has demonstrated the powerful indicator of linking the historical evolution of the landscape, quantified using images, to the observed trends in the hydrochemical composition of stream waters, to highlight the internal processes of the critical zone. However, because of nested effects, it still remains a challenge to strictly quantify their respective impact on streamwater chemistry.

【 授权许可】

Unknown