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3种复合种植模式对退化红壤质量恢复的初探 被引量:11
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作者 拜得珍 纪中华 +2 位作者 杨艳鲜 方海东 廖承飞 《水土保持学报》 CSCD 北大核心 2005年第1期160-163,167,共5页
为了探讨在金沙江干热河谷不同复合种植模式与对退化红壤质量恢复效果方面的关系,以土壤物理性肥力、化学性肥力、蓄水能力、土壤剖面特性和生物治理效益为指标,进行分析和研究。结果表明:(1)退化红壤经过各模式治理后,土壤理化性质得... 为了探讨在金沙江干热河谷不同复合种植模式与对退化红壤质量恢复效果方面的关系,以土壤物理性肥力、化学性肥力、蓄水能力、土壤剖面特性和生物治理效益为指标,进行分析和研究。结果表明:(1)退化红壤经过各模式治理后,土壤理化性质得到改善,通气孔隙度和>1mm团聚体都增加,容重分别是对照区的0.89倍、0.83倍和0.93倍,明显降低。(2)治理、恢复3年,种植模式木豆+酸角、柱花草+酸角、象草+酸角,0~30cm土层有机质分别较对照地增加1.76倍、1.74倍和1.09倍,全氮和有效养分增加幅度也很大。(3)在同一施肥状态下,各模式土壤营养元素在水平和垂直空间土层内都存在明显差异,并且表层土壤理化性质明显好于深层土壤理化性质。(4)各模式经济效益明显增加,分别是对照地的54倍、10倍和28倍;土壤实际蓄水效益也是对照的16.0倍、7.0倍和4.2倍,处理1最高土壤水分滞留量达2.7×104t/hm2,水土保持效益明显。综合各治理指标,发现木豆+酸角模式对改良退化红壤质量取得的综合效益最明显。 展开更多
关键词 退化红壤 复合种植模式 金沙江干热河谷 土壤恢复 土壤肥力 蓄水能力 土壤剖面特性
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The effects of soil sand contents on characteristics of humic acids along soil profiles
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作者 Xinyue Di Hui Dong +2 位作者 Xianjin An Haiming Tang Baohua Xiao 《Acta Geochimica》 EI CAS CSCD 2016年第3期251-261,共11页
It is generally accepted that the compositions and properties of soil organic matter (SOM) are influenced by many factors. In order to reveal the effects of soil texture on characteristics and dynamics of SOM and it... It is generally accepted that the compositions and properties of soil organic matter (SOM) are influenced by many factors. In order to reveal the effects of soil texture on characteristics and dynamics of SOM and its sub-fraction, humic acid (HA), along two soil profiles, a yellow soil profile and a purplish soil profile, under the same climate and vegetation conditions were determined. Results indi- cate that the decomposition and humification degrees of SOM and HA of the purplish soils are higher than those of the corresponding yellow soils indicated by A/O-A ratios of HAs, TOCs and HA yields of bulk soil samples, neverthe- less, the development degree of the purplish soil is lower than that of the yellow soil. The variations of E4/E6 ratios of HAs along the soil profiles indicate the overall molecular sizes of HAs decreased downward along the soil profiles. A/O-A ratios of HAs decreased downward along both the soil profiles indicate that humification processes decrease downward along both the soil profiles. Leaching of SOM shows significant effects on the distribution and character- istics of HAs in the yellow soil profile but the purplish soil profile, which is consistent with the higher hydrophobicity of HAs in purplish soils, shows that the distribution char- acteristics of SOM along the soil profiles are a complex result of the combination of soil texture and characteristics of SOM itself. The remarkably different sand contents are concluded tentatively as one of reasons to the differentdistributions and dynamics of HAs along the soil profiles, however, to profoundly understand the evolution and transport of SOM along soil profiles needs more researches. 展开更多
关键词 Soil profile Soil organic matter Humic acid CHARACTERISTICS Sand content
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