宁南山区苜蓿地土壤水分和养分变异规律研究
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国家自然科学基金项目“宁南黄土丘陵区苜蓿旱化特征及其对土壤养分与微生物的影响”(41061034);国家“十一五”科技支撑计划项目“半干旱黄土丘陵区退化生态系统恢复技术研究”(2006BAC01A07);宁夏自然科学基金(NZ0969)


Variations of Soil Moisture and Nutrients in Alfalfa Field in Southern Ningxia Hui Autonomous Region
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    摘要:

    以宁南半干旱黄土丘陵区3年生、7年生、11年生、19年生,以及7年生上坡、中坡、下坡苜蓿地为研究对象,分析了苜蓿地0—5m土壤干层及土壤养分的消长规律。研究结果表明:(1)坡位与种植年限均对土壤水分产生影响,上坡苜蓿地0—5m土壤平均含水量为6.34%,显著小于中坡和下坡;不同旱作年限苜蓿地0—5m土壤含水量排序为:3年生>7年生>19年生>11年生;土壤干燥化指数SDI排序为:上坡>中坡>下坡;3年生>7年生>19年生>11年生,土壤干燥化程度随着土层深度的增加而减弱。待苜蓿老化后土壤水分可以得到恢复,土壤干燥化程度降低,但这一过程需要较长的时间。(2)在土壤旱化过程中,随着坡位的下降,苜蓿地0—100cm层土壤平均有机质、全氮、速效氮、全磷、速效磷、速效钾含量增加;随着土层深度的增加,土壤有机质、全氮、速效氮、全磷、速效磷下降。随着苜蓿旱作时间的延长,土壤有机质、全氮、速效氮、速效磷、全磷、速效磷含量呈下降的趋势;待苜蓿老化严重时,土壤有机质、全氮开始逐渐积累,但仍然处于低水平状态。

    Abstract:

    In the semi-arid hilly region of South Ningxia Hui Autonomous Region,three-year,seven-year,eleven-year,and nineteen-year old alfalfa fields and seven-year old alfalfa fields at uphill,middle slope,and downhill were taken as study objects.The dynamics of the dried soil layer(0—5 m) and soil moisture and nutrients were analyzed.The results show that both slope position and plant age affected soil moisture contents.The average moisture content of 0—5 m soil profile on the uphill alfalfa field was 6.34%,which was substantially lower than that on middle slope and downhill fields.The average moisture contents in 0—5 m soil profile decreased on the alfalfa fields as in order of three-year,seven-year,nineteen-year,and eleven-year,and soil drying index(SDI) decreased as in order of uphill,middle slope,downhill and three-year,seven-year,nineteen-year,and eleven-year.The dying degree declined as soil depth increased.After the alfalfa aged,soil moisture content could recover but took a long time.On all the alfalfa fields in this study,the average content of soil organic matter,total N,available N,total P,available P,and available K all increased in the fields from uphill to downhill.As the soil depth increased,the soil organic matter,total N,available N,total P,and available P decreased.As the age of alfalfa increased,the soil organic matter,total N,total P,available P,and available K exhibited a declining trend,but the available N increased first and then decreased with the age of alfalfa in the field.When alfalfa field was very old,the soil organic matter and total N began to accumulate but was still at a relatively low level.

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潘占兵,李生宝,蔡进军,董立国,王月玲,季波.宁南山区苜蓿地土壤水分和养分变异规律研究[J].水土保持通报,2011,(2):61-67

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  • 收稿日期:2010-07-15
  • 最后修改日期:2010-08-29
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  • 在线发布日期: 2014-11-26
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