Haoming Fan

Shenyang Agricultural University

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Lili Zhou

Shenyang Agricultural University

Yanfeng Jia

Xinjiang University

Renming Ma

Shenyang Agricultural University

Donghao Huang

Shenyang Agricultural University

Cai Qiang-guo

Chinese Academy of Sciences

Lin Su

Institute of Information Engineering

Congtan Liu

Shenyang Agricultural University

Yu Jiang

St. Jude Children's Research Hospital

Ming Cui

Florida State University

Chen Yang

Princeton University

Cooperative Institutions

Shenyang Agricultural University

Chinese Academy of Sciences

Wageningen University & Research

Nanjing University

Institute of Soil and Water Conservation

University of Chinese Academy of Sciences

Chinese Academy of Medical Sciences & Peking Union Medical College

Chinese Academy of Agricultural Sciences

Beijing Normal University

Sichuan University

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Response mechanism of black soil structure to compound erosion forces in sloping farmland, Northeast China

Soil and Tillage Research (2024)

Yuan Cheng Haoming Fan

10.1016/j.still.2024.106103

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Citations (5)

Linking pore structure characteristics to soil strength and their relationships with detachment rate of disturbed Mollisol by concentrated flow under freeze–thaw effects

Journal of Hydrology (2023)

Бо Лю Haoming Fan Yuzhe Jiang Renming Ma

Snowmelt

Flume

Soil structure

Shear Strength

Mollisol

10.1016/j.jhydrol.2022.129052

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Citations (17)

Effects of pore structure characterized by synchrotron-based micro-computed tomography on aggregate stability of black soil under freeze-thaw cycles

Soil and Tillage Research (2020)

Renming Ma Yu Jiang Bo Liu Haoming Fan

Soil structure

Topsoil

10.1016/j.still.2020.104855

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Citations (98)

Gully erosion susceptibility assessment using three machine learning models in the black soil region of Northeast China

CATENA (2024)

Congtan Liu Haoming Fan Yixuan Wang

Gully Erosion

10.1016/j.catena.2024.108275

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Citations (1)

Effects of Freeze–Thaw Cycles on Brown Forest Soil Available Phosphorus in Northeastern China

Communications in Soil Science and Plant Analysis (2013)

Duo Qian Haoming Fan Lili Zhou Min Wu Ping Guo

Frequently occurring freeze–thaw events can affect soil nutrients. Available phosphorus (AP) is one of the most important plant nutrients in a brown forest soil. Initial soil moisture (15%, 20%, 25%, and 30%), fertilizer concentrations [0, 20, 40, and 60 ppm monopotassium phosphate (KH2PO4)], and freeze–thaw cycles (0, 1, 3, and 6) were considered to determine the effects of freeze–thaw events on AP, and the results indicated that (1) when variables initial soil moisture and fertilizer concentrations were defined, AP concentrations decreased with the increase of freeze–thaw cycles; (2) when variables freeze–thaw cycles and fertilizer concentrations were defined, AP concentrations presented decreased trend with the increase of initial soil moisture, especially initial soil moisture increase from 20% to 30%; and (3) when variables freeze–thaw cycles and initial soil moisture were defined, freeze–thaw events has more obvious influence on AP concentrations in soil samples with no fertilization added than mixed monopotassium phosphate (KH2PO4) before experiment.

Soil test

10.1080/00103624.2013.803567

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Citations (12)

TRACE ELEMENT AND Sr-Nd ISOTOPE GEOCHEMISTRY OF FLUORITE FROM THE XIANGSHAN URANIUM DEPOSIT, SOUTHEAST CHINA

Economic Geology (2006)

Yao-Hui Jiang Huang Ling Songyan Jiang W. Shen Haoming Fan

The trace element and Sr-Nd isotope geochemistry of fluorite have been investigated in the Xiangshan volcanic rock-hosted uranium deposit in southeast China. Detailed Sr-Nd isotope data of the hydrothermal fluorite closely associated with the uranium mineralization suggest that ore-forming fluids were a combination of mantle-derived fluid and fluids equilibrated with basement metamorphic rocks. This model is consistent with previously published H-O isotope data and is incompatible with meteoric water as the only ore-forming fluid. Trace element geochemical profiles across the uranium orebody can be interpreted to reflect reaction between the host rocks and a mantle-derived fluid containing high U and Th with low Th/U ratios. The mantle-derived fluid is considered to have been U-, F- and carbonate-rich. Mixing with shallowly circulated meteoric water within the fractures of the host volcanic rocks caused dilution and cooling of the ore-forming fluid and subsequent precipitation of fluorite and uranium ore.

Fluorite

Trace element

Isotope Geochemistry

Uranium ore

10.2113/gsecongeo.101.8.1613

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Citations (47)

Evaluation of soil macro-aggregate characteristics in response to soil macropore characteristics investigated by X-ray computed tomography under freeze-thaw effects

Soil and Tillage Research (2022)

Bo Liu Haoming Fan Yu Jiang Renming Ma

Macropore

Soil structure

Mollisol

10.1016/j.still.2022.105559

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Citations (28)

Study on Criterion of Soil Loss Tolerance and Soil and Water Conservation in Black Soil Region of Northeast

Journal of Soil and Water Conservation (2006)

Haoming Fan Cai Qiang-guo

The concept and significance of the soil loss tolerance has been reviewed firstly,and then the shortcoming of the loss tolerance criteria being used in the black soil region of northeast China has been pointed out.In referencing to the experience in the world,the soil-forming process,the type and intension of soil loss and the depth of soil are the primary factors to constitute the loss tolerance criteria in the black soil region of northeast China,and especially,the high-point of soil loss control at present and a period of time in the future has been used as a most important factor for loss tolerance criteria constitution.Comprehensive analyzing the investigation result of soil and water conservation practice at 72 small watersheds in the black soil region of northeast China,the criteria of soil loss tolerance and soil loss control has been constituted for the primary soil erosion typical areas.

Source

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Citations (5)

Estimating low eroded sediment concentrations by turbidity and spectral characteristics based on a laboratory experiment

Environmental Monitoring and Assessment (2020)

Xiuquan Xu Haoming Fan Chen Xiao-Yu Mi CaiHong

Turbidity

Soil test

10.1007/s10661-020-8092-x

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Citations (5)

Condition of Soil Erosion in Phaeozem Region of Northeast China

Journal of Soil and Water Conservation (2004)

Haoming Fan Cai Qiang-guo

The relationships between the soil erosion of phaeozem in the northeast region of china and humus, soil parent material, climatic condition, land feature, vegetation and man′s activity in this area have been analyzed. It has been pointed out that the reclamation on a large scale in the phaeozem region is the primary reason causing soil erosion in this place, and at the same time, several natural factors that are the potential factors to affect soil erosion have played more significance role in accelerated erosion after human broke into the phaeozem region. In fact, the phaeozem region of northeast China has became the most hazard region of potential erosion now for it′s unique physical geography environment and man′s activity. At present, the phaeozem region is subjected to severely soil erosion and at somewhere the loess mother material is exposing to the air. So we must action now to explore the law of soil erosion and to cure the soil erosion using this law, or else, the phaeozem region of northeast China will became the real barren land.

Humus

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Citations (37)