Results 21 to 30 of about 203,132 (162)
, 2011 为了解长期种植果树对黄土高原沟壑区土壤水分的影响,对不同种植年限的塬面果园土壤水分特征进行了分析。结果表明:黄土沟壑区塬面果园土壤水分含量普遍低于80%田间持水量,水分较亏缺。0~10 m果园土壤平均含水量与3 m以下各层含水量均呈极显著相关关系,与2~3 m层含水量呈显著相关关系,与0~2 m层次的土壤含水量相关性不显著。土壤水分含量随种植年限的增加呈现先降低后又略有恢复的趋势,但水分恢复量不大。土壤水分波动性及其亏缺量随种植年限的增加呈现先增加后减小的抛物线型变化趋势 ...
谢永生[2], 张义[1,2], 郝明德[2]
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Functional Ecology, Volume 40, Issue 7, Page 2128-2142, July 2026.Read the free Plain Language Summary for this article on the Journal blog. Abstract Soil organic nitrogen (SON) transformation is critical for global nutrient cycling and ecosystem productivity, yet how its responsiveness to climate change differs across diverse land use types remains poorly resolved.
Xinyi Yang +10 more
wiley +1 more source
, 1978 本书由南京土壤所主编，我所参加了垆土、黑垆土和绵土、土壤水分、土壤颗粒等章节的编写。着重论述了西北黄土高原地区成土过程、特点以及垆土、黑垆土和黄绵土的特征和分布规律，把黄土高原区成土过程归为土壤腐殖质累积；石灰的淋溶与淀积；粘化作用；旱耕熟化作用等四个阶段。指出土壤颗粒组成是土壤质地分类依据的基础，在我国北方地区，应着重以砂粒及粗粉粒进行质地分类。在南方地区，应着重以粘粒及粗粉粒进行质地分类。论述了我国土壤水分循环类型的地理分布规律和主要土类的水文状况，土壤有效水和作物生长适宜湿度。另外，主要从增加入渗，
朱显谟, 李玉山, 田积莹
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Functional Ecology, Volume 40, Issue 7, Page 2221-2236, July 2026.Read the free Plain Language Summary for this article on the Journal blog. Abstract Anthropogenic nitrogen (N) deposition is a major driver of global change. However, its effects on the developmental plasticity of plant nutrient strategies remain poorly understood.
Quan Li +11 more
wiley +1 more source
Shuitu Baochi Xuebao, 2007 土壤微生物数量、土壤酶活性可以反映土壤的肥力状况。本文研究了东营泥质海岸不同林分下土壤养分、微生物数量、土壤酶活性及分布特征,结果表明：①土壤微生物、土壤酶和土壤养分主要分布在0-20 cm的土层,20-50 cm的较少;②不同林分微生物数量差异显著。白蜡林微生物数量最多,柳林、枣园数量较少,柽柳林数量最少。③不同林分土壤酶的活性表现出差异性,各种酶之间过氧化氢酶活性最高;④土壤养分含量差异显著,柳林土壤养分含量相对较高于其它样地,白蜡和桑园土壤养分含量次之 ...
李春艳 +5 more
doaj
OnomázeinAlthough å§å§ /jiejie/ (“elder sister”) and 妹妹 /meimei/ (“younger sister”) are basic relatives' terms of the nuclear and consanguinity kinship, they mean a big challenge when they are translated into Spanish because of the linguistic and cultural differences and defaults between the Chinese and the Spanish.
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The underappreciated roles of fog and dew on vegetation and biocrusts
New Phytologist, Volume 251, Issue 1, Page 46-63, July 2026.Summary Fog and dew represent minor components of ecosystem water budgets in most ecosystems. However, fog and dew can play an essential role in ecosystem dynamics and are particularly important for water‐limited systems. In addition to serving as direct water inputs, fog and dew can influence microclimate and water redistribution, thereby promoting ...
Lixin Wang, Yue Li, Mengyun Sun, Na Qiao
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Shuitu Baochi Xuebao, 2002 土壤质量是现代土壤学研究的前沿领域，它不仅注重土壤在生态系统内支撑生物生产力、保持环境质量的功能，而且还强调食物安全和动植物的健康。近年来，土壤质量问题为国内外土壤学研究的热点，就土壤质量的概念、评价指标、土壤质量与生产力、土壤质量与环境质量及动物、人类健康等方面进行了研究及报导。土壤质量物理指标是土壤最基本的质量指标，土壤结构是土壤质量物理指标重要内容，他控制了生态系统内的许多功能，特别是在黄土高原地区，土壤为化学物质成分均一且抗侵蚀较弱的黄土，土壤结构特性决定了该区土壤质量的主要功能 ...
贺秀斌 郑粉莉 李占斌 张成娥 唐克丽
doaj
Functional Ecology, Volume 40, Issue 6, Page 1725-1739, June 2026.Read the free Plain Language Summary for this article on the Journal blog. Abstract Root exudates play a key role as signals and nutrients in mediating plant–microbe communication. However, critical knowledge gaps remain regarding how root exudates mediate soil–microbe–plant interactions to regulate crop yield under long‐term straw mulching combined ...
Jiajie Song +7 more
wiley +1 more source
Shuitu Baochi Xuebao, 2006 分析研究了贵州乌江流域不同喀斯特生态系统的石灰土（岩性均腐土）土壤物理性质。结果表明：喀斯特生态系统（土壤利用方式和土壤侵蚀状况等）是影响土壤物理性质的主要因素。良好生态系统的土壤剖面发育良好，层次分异较明显，土层较深厚；土壤有机质含量较高；以粘壤土和粘土为主；土壤容重适宜，土壤孔隙性和结构性良好，土壤的抗蚀性和抗冲性强。退化生态系统（裸地）的土壤各种物理性状恶化，土壤的抗蚀性和抗冲性减弱。提出评价不同喀斯特生态系统的土壤抗蚀性的主要指标，并得出不同喀斯特生态系统的土壤抗蚀能力依次为：灌丛＋弱度侵蚀 ...
何腾兵 +9 more
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