Dynamics of dissolved iron under pedohydrological regime caused by pulsed rainfall events in wetland soils

Geoderma

Volumn 150, Issue 1-2, 2009, Pages 46-53

  Zou, Yuanchun ^a,b   Lu, Xianguo ^a   Jiang, Ming ^a  

^a NORTHEAST INSTITUTE OF GEOGRAPHY AND AGRICULTURAL ECOLOGY   (China)

^b UNIVERSITY OF CHINESE ACADEMY OF SCIENCES   (China)

Author keywords

Dissolved iron; Drying and wetting cycles; Pedohydrological regime; Pulsed rainfall events; Wetland soil

Indexed keywords

DEWATERING; DISSOLUTION; DYNAMICS; IRON COMPOUNDS; PHOSPHORUS; SOIL MOISTURE; WETTING;

CHEMICAL PARAMETERS; DISSOLVED IRON; ENVIRONMENTAL BEHAVIORS; ENVIRONMENTAL FATES; IN-SITU; INFLUENCING FACTORS; MARSH SOILS; MEADOW MARSHES; NORTHEAST CHINAS; PADDY FIELDS; PEDOHYDROLOGICAL REGIME; PH RESPONSE; POSITIVE CORRELATIONS; PULSED RAINFALL EVENTS; REDOX INDICATORS; REDOX POTENTIALS; SANJIANG PLAINS; SOIL LAYERS; TOTAL CARBONS; TOTAL NITROGENS; TOTAL PHOSPHORUS; WETLAND SOIL;

WETLANDS;

DISSOLVED MATTER; ENVIRONMENTAL FATE; HYDROLOGICAL RESPONSE; IRON; MARSH; MEADOW; PADDY FIELD; RAINFALL; SOIL WATER; WETLAND;

CAREX LASIOCARPA;

EID: 62049083790     PISSN: 00167061     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.geoderma.2009.01.010     Document Type: Article

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