Soil organic nitrogen variation shaped by diverse agroecosystems in a typical karst area: evidence from isotopic geochemistry

TL;DR

This study explores how different land uses in a karst region affect soil organic nitrogen levels and isotopic signatures, showing that grazing shrublands have higher nitrogen content than croplands and forests.

Contribution

The study provides new insights into how diverse agroecosystems influence soil organic nitrogen dynamics using isotopic geochemistry in a karst region.

Findings

Grazing shrublands had significantly higher soil organic nitrogen (SON) content (mean: 0.31%) compared to secondary forest and abandoned cropland.

Goat excreta enriched with 15N contributed to higher δ15NSON values in grazing shrublands.

Long-term cultivation reduces SON, while moderate grazing can enhance it and reduce soil degradation risks.

Abstract

Soil organic nitrogen (SON) levels can respond effectively to crop metabolism and are directly related to soil productivity. However, simultaneous comparisons of SON dynamics using isotopic tracing in diverse agroecosystems are lacking, especially in karst areas with fragile ecology.

To better understand the response of SON dynamics to environmental changes under the coupling of natural and anthropogenic disturbances, SON contents and their stable N isotope (δ15NSON) compositions were determined in abandoned cropland (AC, n = 16), grazing shrubland (GS, n = 11), and secondary forest land (SF, n = 20) from a typical karst area in southwest China.

The SON contents in the SF (mean: 0.09%) and AC (mean: 0.10%) profiles were obviously lower than those in the GS profile (mean: 0.31%). The δ15NSON values ranged from 4.35‰–7.59‰, 3.79‰–7.23‰, and 1.87‰–7.08‰ for the SF, AC, and GS profiles, respectively. Decomposition of organic matter controlled the SON variations in the secondary forest land by the covered vegetation, and that in the grazing shrubland by goat excreta. δ15NSON ranges were controlled by the covered vegetation, and the δ15NSON fractionations during SON transformation were influenced by microorganisms in all surface soil.

The excreta of goats that contained 15N-enriched SON induced a heavier δ15NSON composition in the grazed shrubland. Long-term cultivation consumes SON, whereas moderate grazing increases SON content to reduce the risk of soil degradation. This study suggests that optimized crop-livestock production may benefit the sustainable development of agroecosystems in karst regions.

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