| 引黄灌淤耕作对剖面土壤有机质组分构成的影响 |
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| 引用本文： | 董林林,张海东,于东升,史学正,郭乃嘉,任 杨,张 丽.引黄灌淤耕作对剖面土壤有机质组分构成的影响[J].土壤学报,2017,54(3):613-623. |
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| 作者姓名： | 董林林 张海东 于东升 史学正 郭乃嘉 任 杨 张 丽 |
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| 作者单位： | 1. 土壤与农业可持续发展国家重点实验室(中国科学院南京土壤研究所),南京 210008;苏州市农业科学院,江苏苏州 215155;2. 土壤与农业可持续发展国家重点实验室(中国科学院南京土壤研究所),南京,210008;3. 中宁县农业技术推广服务中心,宁夏中宁,751200 |
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| 基金项目： | 国家自然科学基金项目（面上项目，重点项目，重大项目）;中国科学院重大资助项目 |
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| 摘 要： | 土壤有机质组分构成是影响土壤有机碳库稳定性最直接的原因。为研究灌溉耕作对不同组分土壤有机质含量变化产生的影响,以宁夏引黄灌区为研究对象,通过密度分组方法,测定并分析土壤轻组和重组有机碳含量的变化。结果表明,经过不同时间的引黄灌溉耕作后,土壤轻组和重组有机质含量增加,但是不同组分,其变化量之间存在差异。在剖面深度上,土壤轻组和重组有机质含量及其增加量均随土层深度的增加而降低,表层土壤轻组和重组有机质增加最显著,土壤有机质组分含量的变化受土壤类型的影响明显。与未受灌溉耕作影响的自然土壤相比,灌溉土壤0~60 cm深度内轻组有机质与总有机质间的相关性增强,而且这种相关性随土层深度增加而减弱;自然土壤和灌溉土壤剖面各层次重组有机质与总有机质间均有极强的相关性,说明重组有机质是土壤有机质最为重要的组分,但轻组有机质对灌溉耕作的响应更加敏感,重组有机质较轻组有机质具有更好的固碳效果。
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| 关 键 词： | 引黄灌溉 土壤 轻组有机质 重组有机质 |
| 收稿时间： | 2016/6/16 0:00:00 |
| 修稿时间： | 2016/12/9 0:00:00 |
Effect of cultivation and irrigation with sediment laden Yellow River water on SOM composition in profile depth |
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| DONG Linlin,ZHANG Haidong,YU Dongsheng,SHI Xuezheng,GUO Naiji,REN Yang and ZHANG Li.Effect of cultivation and irrigation with sediment laden Yellow River water on SOM composition in profile depth[J].Acta Pedologica Sinica,2017,54(3):613-623. |
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| Authors: | DONG Linlin ZHANG Haidong YU Dongsheng SHI Xuezheng GUO Naiji REN Yang and ZHANG Li |
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| Institution: | Institute of Soil Science, Chinese Academy of Sciences,Institute of Soil Science, Chinese Academy of Sciences,Institute of Soil Science, Chinese Academy of Sciences,Institute of Soil Science, Chinese Academy of Sciences,Institute of Soil Science, Chinese Academy of Sciences |
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| Abstract: | Objective]Soil organic carbon(SOC),which is the largest storage of organic carbon in the terrestrial ecosystem,is subject to influences of a number of factors,such as climate,geography, human activities,etc. Irrigation is an effective measure to ensure crop production as well as to increase SOC content,particularly,in arid and semiarid areas. Northwest China is an area that has a long history of irrigation with sediment laden river water,where a special layer of anthropogenic soil or irrigation-silt has formed. The layer is quite uniform in soil color,composition,texture,calcium carbonate content,and organic carbon content. When the layer of irrigation-silted is ≥50 cm in thickness,it is termed as irrigation-silted soil. The soil is ≥4 g kg-1 in SOC content,even at the bottom of the irrigation-silted layer. Composition of the soil organic matter(SOM)in fraction,heavy or light is the major factor affecting stability of the SOC storage in the layer.Method]An irrigation zone in Ningxia Province,Northwest China,was selected in the study to evaluate effects of cultivation and irrigation with sediment laden Yellow River water on content and fractionation of SOC. The Yellow River flows through northern part of Ningxia from south to north. Irrigated-alluvial soil,Light sierozem soil,Aeolien sandy soil,Fluvi-aquic soil and Fluvent soil are the types of soils commonly distributed in the Zone. Based on that,a total of 45 soil profiles were specified,including 6 in non-cultivated and non-irrigated natural fields as control,and 39 in irrigated fields different in irrigation history. Each profile was divided into four layers(0~20,20~30,30~60 and 60~100 cm). Soil samples were collected from the layers for analysis of SOC content and for fractionations of SOC,light and heavy by density using 1.7 g m3 NaI solution,so as to illustrate effects of the irrigation with Yellow River water on content and fractionation of SOC. Result]Both light and heavy SOMs were found to have increased in content after years of irrigation,but the increment varied with the duration of irrigation and the fraction. The longer the history of irrigation,the higher the content of both light and heavy OMs in the soil regardless of type. As a result of farming cultivation,including fertilizer or manure application,the contents of OM increased the most significantly(p<0.001)in the plow or surface layer(0~20 cm),and the content and the increment declined along the profile and varied with the type of soil. Irrigated-alluvial soil with a long history of irrigation was found to be highest in OM content,which implies that soil type is another important factor influencing accumulation of SOM. Compared to non-irrigated and non-cultivated soils,irrigated soils exhibited a close relationship between the fraction of light OM and the total SOM in the 0~60 cm soil layer, and the relationship weakened with increasing soil depth,but a very close relationship was found between the fraction of heavy SOM and the total SOM in all the soil layers of both irrigated and non-irrigated fields, which indicates that heavy organic matter is the major component of SOM and accumulates more rapidly than light organic matter. Conclusion]Irrigation with sediment laden Yellow River water helps increase SOC storage,either light or heavy in the Ningxia Irrigation Zone. Heavy OM is the major component of SOM,while light OM is more sensitive to cultivation and irrigation. And the former plays a better role than the latter does in sequestrating soil carbon. |
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| Keywords: | Irrigation withYellow River water soil Light fraction organic matter Heavy fraction organic matter |
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