{"title":"中国西北半干旱高海拔草地土壤湿度对土壤呼吸作用温度响应的阈值","authors":"Zhimin Zhao, Fengxia Shi","doi":"10.1134/s1064229324600143","DOIUrl":null,"url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Abstract</h3><p>Although soil temperature (<i>T</i><sub>s</sub>) is generally considered as the primarily factor influencing soil respiration (<i>R</i><sub>s</sub>), the correlation between soil respiration and soil temperature is often affected by soil moisture (<i>M</i><sub>s</sub>). In this study, we analyzed the correlation between <i>R</i><sub>s</sub> and <i>T</i><sub>s</sub> under different soil moisture condition in semiarid high-altitude grassland in northwestern China. The results showed that (1) when the values of <i>M</i><sub>s</sub> were higher than the field capacity (FC), <i>R</i><sub>s</sub> were mainly controlled by <i>M</i><sub>s</sub>. (2) FC was also an important threshold to affect the selection of <i>R</i><sub>s</sub>–<i>T</i><sub>s</sub> model and the determination of temperature sensitivity (<i>Q</i><sub>10</sub>). Our findings highlight that <i>R</i><sub>s</sub> is significantly influenced by <i>M</i><sub>s</sub> in a threshold manner, and FC is an important moisture threshold for <i>R</i><sub>s</sub> and its temperature response in high altitude semiarid ecosystems.We suggested that the effect of <i>M</i><sub>s</sub> on <i>R</i><sub>s</sub> cannot be neglected in high altitude semiarid ecosystems.</p>","PeriodicalId":11892,"journal":{"name":"Eurasian Soil Science","volume":null,"pages":null},"PeriodicalIF":1.4000,"publicationDate":"2024-07-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Thresholds of Soil Moisture on the Temperature Response of Soil Respiration in Semiarid High-Altitude Grassland in Northwestern China\",\"authors\":\"Zhimin Zhao, Fengxia Shi\",\"doi\":\"10.1134/s1064229324600143\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<h3 data-test=\\\"abstract-sub-heading\\\">Abstract</h3><p>Although soil temperature (<i>T</i><sub>s</sub>) is generally considered as the primarily factor influencing soil respiration (<i>R</i><sub>s</sub>), the correlation between soil respiration and soil temperature is often affected by soil moisture (<i>M</i><sub>s</sub>). In this study, we analyzed the correlation between <i>R</i><sub>s</sub> and <i>T</i><sub>s</sub> under different soil moisture condition in semiarid high-altitude grassland in northwestern China. The results showed that (1) when the values of <i>M</i><sub>s</sub> were higher than the field capacity (FC), <i>R</i><sub>s</sub> were mainly controlled by <i>M</i><sub>s</sub>. (2) FC was also an important threshold to affect the selection of <i>R</i><sub>s</sub>–<i>T</i><sub>s</sub> model and the determination of temperature sensitivity (<i>Q</i><sub>10</sub>). Our findings highlight that <i>R</i><sub>s</sub> is significantly influenced by <i>M</i><sub>s</sub> in a threshold manner, and FC is an important moisture threshold for <i>R</i><sub>s</sub> and its temperature response in high altitude semiarid ecosystems.We suggested that the effect of <i>M</i><sub>s</sub> on <i>R</i><sub>s</sub> cannot be neglected in high altitude semiarid ecosystems.</p>\",\"PeriodicalId\":11892,\"journal\":{\"name\":\"Eurasian Soil Science\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":1.4000,\"publicationDate\":\"2024-07-10\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Eurasian Soil Science\",\"FirstCategoryId\":\"97\",\"ListUrlMain\":\"https://doi.org/10.1134/s1064229324600143\",\"RegionNum\":4,\"RegionCategory\":\"农林科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"SOIL SCIENCE\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Eurasian Soil Science","FirstCategoryId":"97","ListUrlMain":"https://doi.org/10.1134/s1064229324600143","RegionNum":4,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"SOIL SCIENCE","Score":null,"Total":0}
引用次数: 0
摘要
摘要 虽然土壤温度（Ts）通常被认为是影响土壤呼吸作用（Rs）的主要因素，但土壤呼吸作用与土壤温度之间的相关性往往受到土壤水分（Ms）的影响。本研究分析了中国西北半干旱高海拔草地不同土壤水分条件下 Rs 与 Ts 的相关性。结果表明：（1）当 Ms 值高于田间容纳量（FC）时，Rs 主要受 Ms 控制；（2）FC 也是影响 Rs-Ts 模型选择和温度敏感性（Q10）确定的重要临界值。我们的研究结果表明，在高海拔半干旱生态系统中，Rs受Ms的影响很大，而FC是Rs及其温度响应的重要水分阈值。
Thresholds of Soil Moisture on the Temperature Response of Soil Respiration in Semiarid High-Altitude Grassland in Northwestern China
Abstract
Although soil temperature (Ts) is generally considered as the primarily factor influencing soil respiration (Rs), the correlation between soil respiration and soil temperature is often affected by soil moisture (Ms). In this study, we analyzed the correlation between Rs and Ts under different soil moisture condition in semiarid high-altitude grassland in northwestern China. The results showed that (1) when the values of Ms were higher than the field capacity (FC), Rs were mainly controlled by Ms. (2) FC was also an important threshold to affect the selection of Rs–Ts model and the determination of temperature sensitivity (Q10). Our findings highlight that Rs is significantly influenced by Ms in a threshold manner, and FC is an important moisture threshold for Rs and its temperature response in high altitude semiarid ecosystems.We suggested that the effect of Ms on Rs cannot be neglected in high altitude semiarid ecosystems.
期刊介绍：
Eurasian Soil Science publishes original research papers on global and regional studies discussing both theoretical and experimental problems of genesis, geography, physics, chemistry, biology, fertility, management, conservation, and remediation of soils. Special sections are devoted to current news in the life of the International and Russian soil science societies and to the history of soil sciences.
Since 2000, the journal Agricultural Chemistry, the English version of the journal of the Russian Academy of Sciences Agrokhimiya, has been merged into the journal Eurasian Soil Science and is no longer published as a separate title.
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