Forest Recovery Reduces Production and Rising Aridity Diminishes Export of Dissolved Inorganic Carbon

IF 5 1区 地球科学 Q2 ENVIRONMENTAL SCIENCES
Bingqin Wang, Hang Wen, Bryn Stewart, Li Li, Xi Chen, Si‐Liang Li
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引用次数: 0

Abstract

Riverine dissolved inorganic carbon (DIC), essential for understanding terrestrial carbon cycling, is undergoing dramatic changes due to climate change and human disturbances. Quantifying how these changes impact DIC fluxes from land to rivers has remained challenging due to limited long‐term data and complex, interacting drivers. Here we ask the question: How and to what extent do climate and land‐cover changes distinctively influence long‐term seasonal and annual trends of DIC production and export? We developed a reactive transport model, constrained by three decades of streamflow, DIC, and carbon isotope data, for a karst catchment in southwest China simultaneously experiencing a warmer, drier climate (increasing aridity) and forest recovery. Results show that from 1980 to 2010s, precipitation has declined from 1,261 to 1,005 mm/yr, and discharge from 700 to 552 mm/yr, with no significant change in evapotranspiration. DIC production and export have declined at the rates of 2.3 × 105 and 5.4 × 105 mol C/yr/yr, respectively. Drier climate and reduced discharge diminish carbonate weathering but also store more produced DIC, resulting in higher DIC concentrations over time but a twofold decline in DIC export compared to its production. Interestingly, although forest recovery elevates organic carbon content, cooling soils and lower soil moisture reduce rates of soil respiration. Scenario analysis shows that forest recovery accounts for 91% of the production decline, while increasing climate aridity explains 78% of the export reduction. Seasonal analysis further reveals that soil respiration declines most during hot‐wet seasons but calcite weathering drops more in cold‐dry seasons. These findings underscore the differential impacts of climate and land‐cover changes on carbon transport and transformation processes, which are crucial for understanding carbon cycling and budgets under evolving environmental conditions.
森林恢复减少了产量,干旱加剧减少了溶解无机碳的出口
由于气候变化和人为干扰,河流溶解无机碳(DIC)正经历着剧烈的变化,对了解陆地碳循环至关重要。由于有限的长期数据和复杂的、相互作用的驱动因素,量化这些变化如何影响从陆地到河流的DIC通量仍然具有挑战性。在这里,我们提出了一个问题:气候和土地覆盖变化如何以及在多大程度上显著影响DIC生产和出口的长期季节性和年度趋势?基于30年的河流流量、DIC和碳同位素数据,我们建立了一个反应输运模型,以中国西南喀斯特流域为研究对象,该流域同时经历了气候变暖、干燥(干旱加剧)和森林恢复。结果表明:1980 ~ 2010年代,降水量从1261 mm/yr减少到1005 mm/yr,径流量从700 mm/yr减少到552 mm/yr,蒸散量变化不显著;DIC产量和出口量分别以2.3 × 105 mol C/年和5.4 × 105 mol C/年的速度下降。干燥的气候和减少的排放减少了碳酸盐的风化作用,但也储存了更多产出的DIC,导致DIC浓度随着时间的推移而升高,但DIC的出口与产量相比下降了两倍。有趣的是,虽然森林恢复提高了有机碳含量,但土壤冷却和土壤湿度降低降低了土壤呼吸速率。情景分析表明,森林恢复占产量下降的91%,而气候干旱加剧占出口减少的78%。季节分析进一步表明,土壤呼吸在热湿季节下降最多,而方解石风化在冷干季节下降更多。这些发现强调了气候和土地覆盖变化对碳运输和转化过程的不同影响,这对于理解不断变化的环境条件下的碳循环和预算至关重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Water Resources Research
Water Resources Research 环境科学-湖沼学
CiteScore
8.80
自引率
13.00%
发文量
599
审稿时长
3.5 months
期刊介绍: Water Resources Research (WRR) is an interdisciplinary journal that focuses on hydrology and water resources. It publishes original research in the natural and social sciences of water. It emphasizes the role of water in the Earth system, including physical, chemical, biological, and ecological processes in water resources research and management, including social, policy, and public health implications. It encompasses observational, experimental, theoretical, analytical, numerical, and data-driven approaches that advance the science of water and its management. Submissions are evaluated for their novelty, accuracy, significance, and broader implications of the findings.
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