College of Natural Resources and Environment, Northwest A&F University, Yangling, Shaanxi 712100, China
Key Laboratory of Plant Nutrition and the Agri-Environment in Northwest China, Ministry of Agriculture, Northwest A&F University, Yangling, Shaanxi 712100, China
Junjun Liu
College of Natural Resources and Environment, Northwest A&F University, Yangling, Shaanxi 712100, China
Feinan Hu
State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling, Shaanxi 712100, China
Institute of Soil and Water Conservation, Chinese Academy of Sciences, Ministry of Water Resources, Yangling, Shaanxi 712100, China
Zengchao Geng
College of Natural Resources and Environment, Northwest A&F University, Yangling, Shaanxi 712100, China
Key Laboratory of Plant Nutrition and the Agri-Environment in Northwest China, Ministry of Agriculture, Northwest A&F University, Yangling, Shaanxi 712100, China
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1,070
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1,390
77
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PDF: 197
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Supplement: 77
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Cumulative views and downloads
(calculated since 11 Jun 2024)
Total article views: 868 (including HTML, PDF, and XML)
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717
135
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868
40
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HTML: 717
PDF: 135
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Total: 868
Supplement: 40
BibTeX: 34
EndNote: 55
Views and downloads (calculated since 27 Jan 2025)
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Total article views: 522 (including HTML, PDF, and XML)
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353
62
107
522
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HTML: 353
PDF: 62
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Total: 522
Supplement: 37
BibTeX: 25
EndNote: 20
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Total article views: 1,390 (including HTML, PDF, and XML)
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Total article views: 868 (including HTML, PDF, and XML)
Thereof 810 with geography defined
and 58 with unknown origin.
Total article views: 522 (including HTML, PDF, and XML)
Thereof 503 with geography defined
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The differences in organic matter contents and clay mineralogy are the fundamental reasons for the differences in colloidal suspension stability behind the size effects of Anthrosol and Calcisol colloids. The present study revealed the size effects of two alkaline soil colloids on carbon content, clay minerals, surface properties and suspension stability, emphasizing that soil nanoparticles are prone to be more stably dispersed instead of being aggregated.
The differences in organic matter contents and clay mineralogy are the fundamental reasons for...