Jiahao Qin , Xiaodong Zhang , Shikui Dong , Changxun Yu , Xiaomin Yang , Zimin Li , Danghui Xu , Hailong Wang , Zhaoliang Song
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引用次数: 0
Abstract
Alpine grassland ecosystem plays a vital role in regulating global carbon (C) cycle, being of great importance for mitigating global warming. Applying nitrogen (N) and phosphorus (P) fertilizers illustrates significant effects on alpine grassland service function in Qinghai-Tibetan Plateau (QTP), especially on grassland ecosystem C sink. Phytolith C sequestration, as an important C sink mechanism, has significant contribution to global long-term stable C sink. However, the effects of N and P addition on phytolith C sequestration in alpine grassland ecosystem of QTP are still unclear. We conducted a field experiment with N and P addition treatments in alpine grassland of QTP to analyze their effects on soil properties, plant biomass, phytolith contents, and the occluded C (PhytOC) contents in alpine grassland ecosystem. Experimental results showed that adding N fertilizers (72 kg ha−1 yr−1) significantly increased the grass phytolith content, with an increase of 29.5 ± 17.5 % compared to the control, and with a 12.9 ± 9.1 % increase with adding P fertilizers (36 kg ha−1 yr−1). In contrast, the co-addition of N and P increased the soil phytolith and PhytOC contents (0–10 cm) by 40.9 ± 14.4 % and 58.9 ± 1.6 %, respectively. Yet excessive N addition reduced the contents of soil phytolith and PhytOC due to soil acidification and nutrient imbalances. In addition, both soil organic C and soil available silicon had significant positive correlation with soil phytolith contents, while soil pH and ammonium N had significant negative correlation with soil phytolith contents. These findings reveal that adding N and P regulates the long-term stable C sequestration in alpine grassland ecosystem via promoting the accumulation of phytoliths and phytolith C storage. Our findings provide the main scientific reference for the management of alpine grassland ecosystem on the QTP.
高寒草地生态系统在调节全球碳(C)循环中起着至关重要的作用,对减缓全球变暖具有重要意义。植物岩固碳作为一种重要的碳汇机制,对全球长期稳定的碳汇有重要贡献。然而,氮磷添加对青藏高原高寒草地生态系统植物岩碳固存的影响尚不清楚。通过对青藏高原高寒草地的田间试验,分析了不同施氮加磷处理对高寒草地生态系统土壤性质、植物生物量、植物体含量和封闭碳(PhytOC)含量的影响。结果表明,施用N肥(72 kg ha−1 yr−1)显著提高了草地植石含量,比对照提高了29.5±17.5%,施用P肥(36 kg ha−1 yr−1)显著提高了12.9±9.1%。氮磷共施可使0 ~ 10 cm土壤植石和植物碳含量分别提高40.9±14.4%和58.9±1.6%。过量施氮导致土壤酸化和养分失衡,降低了土壤植石和植物碳含量。土壤有机碳和土壤有效硅与植物体含量呈显著正相关,土壤pH和铵态氮与植物体含量呈显著负相关。上述结果表明,添加N和P通过促进植物岩积累和植物岩碳储量调节高寒草地生态系统长期稳定的碳固存。研究结果为青藏高原高寒草地生态系统的管理提供了重要的科学参考。
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.