Results 31 to 40 of about 894,370 (93)
Shuitu Baochi Xuebao, 2004 不同开垦年限黑土土壤有机碳及其组分含量变化的研究结果表明:土壤开垦前50年,黑土耕层及犁底层总有机碳及其组分含量下降迅速,土壤有机碳的氧化稳定性系数变化强烈。黑土开垦130年后,有机碳及各组分含量基本上处于相对稳定状态。黑土耕作200年,耕层总有机碳含量损失幅度约1.76%～24.81%。有机碳组分中,FA-C受开垦年限影响相对较小,Hu-C受开垦年限影响最大。
于君宝 刘景双 王金达 刘淑霞 齐小宁 王洋 王国平
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Veterinary Dermatology, Volume 36, Issue 3, Page 302-313, June 2025.Background – Malassezia pachydermatis (MP) is implicated in severe dermatitis and otitis externa (OE) of companion animals and recently gained attention for its increasing resistance to azole compounds. For this reason, developing novel therapeutic strategies is of great interest. In a previous work, we used reference yeast isolates to evaluate several
Costanza Spadini +11 more
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Functional Ecology, Volume 39, Issue 5, Page 1274-1287, May 2025.Read the free Plain Language Summary for this article on the Journal blog. Abstract Interactions between plants and soil microorganisms in the rhizosphere are vital for maintaining the nutrient cycle and stability of terrestrial ecosystems. Nitrogen, closely related to carbon (C) cycling and ecosystem productivity, undergoes transformation by soil ...
Ru Wang +9 more
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Shuitu Baochi Xuebao, 2011 调查采集长江荆江段湿地围垦农田土壤的表土样品,实验室分析总有机碳(SOC)、热水溶性有机碳(HWEC)、颗粒态有机碳(POC)、易氧化有机碳(LOC)及有机碳键合组分含量特征,比较分析不同土地利用方式下湿地起源土壤有机碳组分的变化。结果表明,棉田土壤总有机碳含量为(8.86±0.73)g/kg,桔园的为(9.07±0.01)g/kg,湿地的为(10.30±0.37)g/kg,稻田的为(15.57±1.92)g/kg。即棉田和桔园的总有机碳含量接近于湿地的,而稻田的较大幅度高于前面旱地和湿地的。同时 ...
邰继承 +3 more
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温度对贵州喀斯特黄色石灰土有机碳矿化、水稻秸秆激发效应和Q10的影响
Shuitu Baochi Xuebao, 2022 为定量揭示温度和秸秆还田对贵州喀斯特黄色石灰土土壤有机碳矿化、激发效应和温度敏感性的影响。以贵州喀斯特地区典型黄色石灰土为研究对象,采用13C稳定性同位素标记的水稻秸秆和土壤培养试验研究了15,25,35 ℃培养温度下土壤原有有机碳矿化速率、累积矿化量、激发效应和温度系数Q10对水稻秸秆输入和温度的响应。结果表明:15~35 ℃温度范围和0~60天培养时间内,贵州喀斯特黄色石灰土土壤有机碳、总有机碳、水稻秸秆有机碳和土壤原有有机碳矿化速率均培养1天达到峰值,培养1~30天土壤总有机碳 ...
段建军 +6 more
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China's Eco‐Civilisation, Climate Leviathan, and Hobbesian Energy Transition
Antipode, Volume 57, Issue 3, Page 830-861, May 2025.Abstract Scholars have hitherto tended to theorise China's ecological civilisation project either as a form of environmental authoritarianism or as a vision of eco‐socialism. This paper contributes to the conversation by conducting a textual analysis of Chinese scholarly discussions on eco‐civilisation.
David Chen
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Lianas shift towards larger sizes and more acquisitive trait values in an Asian tropical rainforest
Biotropica, Volume 56, Issue 2, March 2024.Liana communities showed a shift in trait values indicating that they changed towards more large, acquisitive lianas with rapid water use. There are more larger stems through time due to the relatively low mortality of the larger individuals, which is associated with relatively low levels of disturbance.
Qi Liu +3 more
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, 2011 系统测定了陕西洛川黑木沟黄土/古土壤的总有机碳及其主要组分(稳定有机碳、矿物保护有机碳和化学稳定有机碳)的含量,并对总有机碳与粘粒含量及粘土矿物含量的相关性进行了分析。结果表明:(1)各层古土壤的总有机碳含量均高于其下伏的黄土层(S4例外),而稳定有机碳、矿物保护有机碳以及化学稳定有机碳的平均含量在黄土与古土壤之间无明显差异;(2)黄土和古土壤中有机碳含量达到稳定所需要的时间不同,分别是140~250 ka和330~410ka;(3)总有机碳和化学稳定有机碳与粘粒呈正相关关系(相关系数r分别为0 ...
孙旭辉[1] +6 more
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Shuitu Baochi Xuebao, 2006 以保护性耕作长期定位试验为研究对象，分析了保护性耕作对土壤不同层次的总碳、活性碳的影响，并计算了各处理的碳库活度、碳库活度指数和碳库管理指数。结果表明，土壤总有机碳和活性碳均随土层的增加而减少，其0～30cm平均总有机碳含量大小为旋耕〉免耕〉翻耕〉对照，秸秆还田提高土壤耕层总有机碳，旋耕和免耕提高表层土壤有机碳．且差异达到显著水平；土壤活性碳平均含量为旋耕〉翻耕〉对照〉免耕，旋耕和翻耕提高土壤活性碳，免耕则降低土壤活性碳，尤其是10～20cm土层活性碳比旋耕下降了27．33％。华北平原0 ...
李琳, 李素娟, 张海林, 陈阜
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, 2008 采用全国第二次土壤普查数据结合作者的实测数据,利用1∶100万土壤数据库对青藏高原土壤有机质层、土壤矿质层及整个剖面的土壤有机碳密度和土壤有机碳储量分别进行了估算。结果表明:青藏高原的平均土壤有机碳密度约为C7.2kgm-2,较前人的C8.01~19.05kgm-2全国平均土壤有机碳密度偏低。青藏高原总的土壤有机碳储量约为18.37Pg,其中有机质层土壤有机碳储量约占38.14%,矿质层土壤有机碳储量则占61.86%。中国科学院知识创新工程重要方向项目(KZCX3-SW-339-04 ...
欧阳华 +4 more
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