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首页|期刊导航|生态学杂志|荒漠-绿洲过渡带不同土地利用类型下土壤有机碳矿化特征及其对氮添加的响应

荒漠-绿洲过渡带不同土地利用类型下土壤有机碳矿化特征及其对氮添加的响应

宋佼阳 赵广兴 丛孟菲 张志浩 曾凡江

生态学杂志2025,Vol.44Issue(8):2506-2514,9.
生态学杂志2025,Vol.44Issue(8):2506-2514,9.DOI:10.13292/j.1000-4890.202508.033

荒漠-绿洲过渡带不同土地利用类型下土壤有机碳矿化特征及其对氮添加的响应

Soil organic carbon mineralization characteristics under different land use types in desert-oasis transition zone and its response to nitrogen addition

宋佼阳 1赵广兴 1丛孟菲 2张志浩 3曾凡江4

作者信息

  • 1. 中国科学院新疆生态与地理研究所,新疆荒漠植物根系生态与植被修复重点实验室,乌鲁木齐 830011||荒漠与绿洲生态国家重点实验室,干旱区生态安全与可持续发展重点实验室,中国科学院新疆生态与地理研究所,乌鲁木齐 830011||新疆策勒荒漠草地生态系统国家野外科学观测研究站,新疆策勒 848300||中国科学院大学,北京 100049
  • 2. 中国科学院新疆生态与地理研究所,新疆荒漠植物根系生态与植被修复重点实验室,乌鲁木齐 830011||荒漠与绿洲生态国家重点实验室,干旱区生态安全与可持续发展重点实验室,中国科学院新疆生态与地理研究所,乌鲁木齐 830011||新疆策勒荒漠草地生态系统国家野外科学观测研究站,新疆策勒 848300||新疆大学,乌鲁木齐 830046
  • 3. 中国科学院新疆生态与地理研究所,新疆荒漠植物根系生态与植被修复重点实验室,乌鲁木齐 830011||荒漠与绿洲生态国家重点实验室,干旱区生态安全与可持续发展重点实验室,中国科学院新疆生态与地理研究所,乌鲁木齐 830011||新疆策勒荒漠草地生态系统国家野外科学观测研究站,新疆策勒 848300
  • 4. 中国科学院新疆生态与地理研究所,新疆荒漠植物根系生态与植被修复重点实验室,乌鲁木齐 830011||荒漠与绿洲生态国家重点实验室,干旱区生态安全与可持续发展重点实验室,中国科学院新疆生态与地理研究所,乌鲁木齐 830011||新疆策勒荒漠草地生态系统国家野外科学观测研究站,新疆策勒 848300||中国科学院大学,北京 100049||新疆大学,乌鲁木齐 830046
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摘要

Abstract

We explored the mineralization potential of soil organic carbon(SOC)between two land use types,shrubland and cropland,in the southern edge of the desert-oasis transition zone in hyper-arid area of the Taklama-kan Desert,and analyzed the response mechanism to nitrogen(N)addition.Adjacent uncultivated desert land was used as a control.NH4Cl was used as the N source.The SOC mineralization rate and cumulative SOC mineralization were measured in an incubation experiment in the laboratory.The regulatory factors of SOC mineralization including the microbial community composition and enzyme activities related to carbon and N cycling were explored.The re-sults showed that land use types had a significant impact on the cumulative mineralization of SOC.The cumulative mineralization of SOC in cropland and shrubland were significantly higher than those in uncultivated desert land(P<0.05).The mineralization rate of SOC peaked on the 1st or 3rd day,and then gradually decreased with the exten-sion of incubation time.The cumulative mineralization of SOC was significantly negatively correlated with soil dis-solved organic N,ammonium,and nitrate,but positively correlated with pH(P<0.05).Redundancy analysis showed that 95.02%of the variation of SOC mineralization was explained by enzyme activity and microbial commu-nity composition,and fungi to bacteria ratio.Gram-positive bacteria and actinomyces abundances exerted the grea-test impact on SOC mineralization.Nitrogen addition delayed the occurrence time of the maximum of soil mineraliza-tion rate in shrublands and uncultivated desert lands,but did not affect soil microbial community composition and SOC cumulative mineralization.These findings indicate that the reclamation of desert lands into shrublands and croplands can increase SOC mineralization,with nutrient availability playing an important role in this process.

关键词

土壤有机碳矿化/土地利用类型/氮添加/酶活性/微生物群落组成

Key words

soil organic carbon mineralization/land use type/nitrogen addition/enzyme activity/microbial com-munity composition

引用本文复制引用

宋佼阳,赵广兴,丛孟菲,张志浩,曾凡江..荒漠-绿洲过渡带不同土地利用类型下土壤有机碳矿化特征及其对氮添加的响应[J].生态学杂志,2025,44(8):2506-2514,9.

基金项目

国家重点研发计划(2022YFF1302504)、国家自然科学基金面上项目(42271071)、天山英才创新领军人才计划(2023TSYCLJ0046)资助. (2022YFF1302504)

生态学杂志

OA北大核心

1000-4890

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