生物结皮的发展改变了旱地土壤多功能性的驱动因素

IF 5.7 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Mingming Wang , Boyi Song , Benfeng Yin , Ye Tao , Jing Zhang , Xiaoying Rong , Yonggang Li , Shihang Zhang , Zihan Kan , Yongxing Lu , Hao Guo , Xing Guo , Wei Hang , Jungang Yang , Fan Du , Yuanming Zhang , Xiaobing Zhou , Jorge Durán
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引用次数: 0

摘要

生物结皮是旱地土壤的重要组成部分,但其发展对土壤多功能性的影响及其背后的驱动因素尚不清楚。我们在中国西北沙漠的11个地点取样,代表了BSC发展的不同演替阶段(即蓝藻、地衣和苔藓结壳)以及裸沙地区。我们评估了不同深度(0-2、2-5、5-10、10-20 cm)下地壳层和土壤的SMF,并探讨了气候因素(年平均温度、干旱和太阳辐射)、地壳特征(抗压强度、粗糙度和厚度)和土壤性质(pH、电导率、土壤含水量)对这些层的SMF的影响。BSCs的存在显著改善了0 ~ 20 cm土壤深度的土壤营养状况[土壤有机碳(SOC)、全氮(TN)、全磷(TP)、氨(NH4+-N)、硝态氮(NO3—N)和速效磷(AP)],增加了0 ~ 10 cm土壤表层的SMF。这些积极作用随着BSCs从蓝藻到地衣再到苔藓阶段的进展而增强,但随着土壤深度的增加而减弱。在地壳层,所有BSC类型的SMF均受到气候因子的正影响。然而,随着BSCs的发展,气候因子(主要是太阳辐射)和土壤性质(主要是pH)对SMF的负面影响减弱,而地壳特征(主要是厚度)对SMF的正面影响增强。气候、结皮和土壤因子对SMF的影响也随土壤深度的增加而减小,且随生态平衡卡类型的不同而不同。此外,我们的研究结果表明,BSC的发展可以缓冲土壤pH和太阳辐射增加对SMF的负面影响,同时增强结壳性质(特别是厚度)的积极影响。这凸显了保护和促进平衡计分卡发展对于增强表层土壤多功能性和减轻气候变化对旱地生态系统多功能性的不利影响的重要性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

The development of biological soil crusts shifts the drivers of soil multifunctionality in drylands

The development of biological soil crusts shifts the drivers of soil multifunctionality in drylands
Biological soil crusts (BSCs) are essential components of drylands, yet the effects of their development on soil multifunctionality (SMF) and the drivers behind these effects remain unclear. We sampled 11 sites in Northwest China’s deserts, representing different successional stages of BSC development (i.e. cyanobacterial, lichen and moss crusts) as well as bare sand areas. We assessed the SMF of the crust layer and underlying soil at various depths (0–2, 2–5, 5–10, 10–20 cm) and also explored the influence of climatic factors (mean annual temperature, aridity, and solar radiation), crust characteristics (compressive strength, roughness, and thickness), and soil properties (pH, electrical conductivity, soil water content) on SMF across these layers. The presence of BSCs significantly enhanced soil nutritional status [soil organic carbon (SOC), total nitrogen (TN), total phosphorus (TP), ammonia (NH4+-N), nitrate (NO3-N), and available phosphorus (AP)] throughout the 0–20 cm soil depth and increased SMF in the top 0–10 cm. These positive effects intensified with as BSCs progressed from cyanobacterial to lichen to moss stages, but decreased with soil depth. In the crust layer, SMF across all BSC types was positively influenced by our climatic factors. However, as BSCs developed, the negative influence of climatic factors (mainly solar radiation) and soil properties (mainly pH) on SMF decreased, while the positive influence of crust characteristics (mainly thickness) increased. The influence of climate, crust, and soil factors on SMF also decreased with increasing soil depth and varied by BSC type. Further, our findings demonstrate that the BSC development can buffer the negative effects of increased soil pH and solar radiation on SMF while enhancing the positive effects of crust properties, particularly thickness. This highlights the importance of preserving and promoting BSC development to enhance surface soil multifunctionality and mitigate the adverse effects of climate change on dryland ecosystem multifunctionality.
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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