Variation in soil organic carbon stock in different land uses and altitudes in Bagrot Valley, Northern Karakoram

Abstract

Soil organic carbon tends to respond more sensitively to climate change and land use intensification in ecologically fragile and economically marginal regions of mountainous areas. This study aims to evaluate the soil organic carbon stock dynamic across various land uses at different altitudes in the Bagrot valley, Northern Karakoram, Gilgit-Baltistan, Pakistan. Soil samples from 0–20, 20–40 and 40–60 cm depth were collected from three land uses: pasture, forest, and adjacently located arable land at different altitude (ranging from 2100–4163 m). The variables investigated were soil bulk density (BD), soil organic carbon concentration (SOC), soil organic carbon stock (SOCS) and pH. A significant variation in all tested variables were found across the land uses and altitudes. Likewise, soil under forest had significantly higher values of SOCS (59.35 Mg ha−1) than pasture (42.48 Mg ha−1) and arable land (23.63 Mg ha−1). Similarly, SOCS increased with increasing altitude and decreased with soil depth in all land uses. In addition, SOCS had a negative relationship with BD and pH. Overall results indicated that the land use intensification and climate change (increase in temperature and decrease in precipitation) were associated with declining SOCS. These results suggest restoration of degraded agricultural land to the forest, especially at higher altitude, and decrease in intensity of land use could increase SOCS in the study area as well as other similar mountainous regions.

Keywords

• bagrot valley
• climate change
• gilgit-baltistan
• mixed mountain agriculture
• vegetation density