金沙江干热河谷不同植被坡面土壤水分时空分布特征
|
摘要
于2016年7～12月和2017年4月的旱、雨季期间,以金沙江干热河谷苴那小流域内的银合欢(Leucaena Benth)林地、车桑子(Dodonaea viscosa)灌丛地和扭黄茅(Heteropogon contortus)草地为研究对象,通过网格法和土钻法采集并测定了(0～100 cm)土层的土壤含水量,应用经典统计法和地统计学方法分析该区域不同林草植被下坡面土壤水分的动态变化特征。结果表明:(1)研究区土壤含水量总体较低,雨季显著大于旱季,旱、雨季均表现为灌丛地>草地>林地,呈中度至强度变异(0. 07～0. 28之间)。(2)不同林草植被下旱、雨季土壤水分具有相似的空间自相关性,自相关系数均由正向负转变,但由正向负转变的滞后距离有所不同,且雨季大于旱季,呈中等或强等空间自相关性。(3)不同林草植被下的土壤水分空间结构不同,林地、灌丛地和草地旱雨季最佳拟合模型均为球状模型;相同林草植被下各土层旱、雨季土壤水分的空间分布特征相似,但旱季的分布格局差异更显著,不同林草植被下深层土壤水分分布比表层土壤水分的分布更为复杂,土壤水分呈明显的斑块或条带状分布,含水量高值区和低值区位置不固定。总之不同林草植被类型会改变局部地段土壤水分空间分布,降雨会加强这种差异的趋势,但土壤水分仍具一定空间连续性。
In order to explore the influence of typical forest grass vegetation on soil moisture change on sloping land in dry hot valley area,the soil moisture content( within the depth of 0 to 100 cm) were collected and measured using the grid sampling method and soil auger method in the drought season in July to December 2016 and rainy season in April 2017,taking the Leucaena Benth forest land,Dodonaea angustifolia shrub land and Heteropogon cantortus grassland as the research objects at dry-hot valley of Juna small watershed in Jinsha River,Yunnan Province,China. The dynamic characteristics of soil moisture under typical forest vegetation in the slope area were analyzed with geostatistics method. The soil moisture content in the dry-hot valley of Jinsha River was low( which were7. 44% in the dry season and 9. 88% in the rainy season for the forest land; 10. 25% and 10. 31% respectively for the shrub land; and 5. 03% and 10. 60% respectively for the grassland),the soil moisture in the rainy season was higher than that in the dry season,and the soil moisture content in the shrub land was bigger than that in the grassland which was bigger than that in the forest land regardless of the dry season or the rainy season,showing a moderate to strong variation( between 0. 07 to 0. 28). The soil moisture in the hot valley of Jinsha has significant spatial structure and spatial continuity,and the soil moisture had similar spatial autocorrelation regardless of the season( drought season or rainy season) and the land cover( forest or shrub or grass vegetation). All the autocorrelation coefficients went from positive to negative but with a different lagging distance in the transformation and it was bigger in the rainy season than that in the dry season,demonstrating a moderate to strong spatial autocorrelation. The spatial structure of soil moisture was different depending on the types of land cover and this difference was remarkable in the dry season. The moisture distribution in the deep soil was more complex than that in the surface layer,displaying an obvious patched or stripped distribution with unset high water content areas and low water content areas.The best fitting model was the spherical model for the forest land,shrub and grassland. Under the same land cover,the spatial structure of the water content was similar regardless of dry season or rainy season. In short,different type of land cover will change the spatial distribution of soil moisture in the areas and the rainfall will amplify this difference,but soil moisture still has some spatial continuity. Therefore,diverse strategies in the utilization of water resources should be adopted during ecological restoration and vegetation reconstruction in dry-hot valley.
In order to explore the influence of typical forest grass vegetation on soil moisture change on sloping land in dry hot valley area,the soil moisture content( within the depth of 0 to 100 cm) were collected and measured using the grid sampling method and soil auger method in the drought season in July to December 2016 and rainy season in April 2017,taking the Leucaena Benth forest land,Dodonaea angustifolia shrub land and Heteropogon cantortus grassland as the research objects at dry-hot valley of Juna small watershed in Jinsha River,Yunnan Province,China. The dynamic characteristics of soil moisture under typical forest vegetation in the slope area were analyzed with geostatistics method. The soil moisture content in the dry-hot valley of Jinsha River was low( which were7. 44% in the dry season and 9. 88% in the rainy season for the forest land; 10. 25% and 10. 31% respectively for the shrub land; and 5. 03% and 10. 60% respectively for the grassland),the soil moisture in the rainy season was higher than that in the dry season,and the soil moisture content in the shrub land was bigger than that in the grassland which was bigger than that in the forest land regardless of the dry season or the rainy season,showing a moderate to strong variation( between 0. 07 to 0. 28). The soil moisture in the hot valley of Jinsha has significant spatial structure and spatial continuity,and the soil moisture had similar spatial autocorrelation regardless of the season( drought season or rainy season) and the land cover( forest or shrub or grass vegetation). All the autocorrelation coefficients went from positive to negative but with a different lagging distance in the transformation and it was bigger in the rainy season than that in the dry season,demonstrating a moderate to strong spatial autocorrelation. The spatial structure of soil moisture was different depending on the types of land cover and this difference was remarkable in the dry season. The moisture distribution in the deep soil was more complex than that in the surface layer,displaying an obvious patched or stripped distribution with unset high water content areas and low water content areas.The best fitting model was the spherical model for the forest land,shrub and grassland. Under the same land cover,the spatial structure of the water content was similar regardless of dry season or rainy season. In short,different type of land cover will change the spatial distribution of soil moisture in the areas and the rainfall will amplify this difference,but soil moisture still has some spatial continuity. Therefore,diverse strategies in the utilization of water resources should be adopted during ecological restoration and vegetation reconstruction in dry-hot valley.
引文
[1] HAUCK C,BARTHLOTT C,KRAUSS L,et al. Soil moisture variability and its influence on convective precipitation over complex terrain[J]. Quarterly Journal of the Royal Meteorological Society,2015,137(S1):42-56.
[2] REN Q S,MA P,LI C X,et al. Evaluation of bacterial diversity under different herb vegetation types in the hydro-fluctuation zone of the Three Gorges Reservoir in China[J]. Acta Ecologica Sinica,2016.
[3] FENG W,YANG W B,TANG J N,et al. Deep soil water infiltration and its dynamic characteristics in Chinese Deserts[J]. Journal of Desert Research,2015.
[4] FU Z Y,LI Z X,CAI C F,et al. Soil thickness effect on hydrological and erosion characteristics under sloping lands:A hydropedological perspective[J]. Geoderma,2011,167(167):41-53.
[5]史志华,朱华德,陈佳,等.小流域土壤水分空间异质性及其与环境因子的关系[J].应用生态学报,2012,23(4):889-895.[SHI Zhihua,ZHU Huade,CHEN Jia,et al. Spatial heterogeneity of soil moisture and its relationships with environmental factors at small catchment level[J]. Chinese Journal of Applied Ecology,2012,23(4):889-895.]
[6] YU F,ZHAO Y S. A new semi-empirical model for soil moisture content retrieval by ASAR and TM data in vegetation-covered areas[J]. Science China Earth Sciences,2011,54(12):1955-1964.
[7]包含,侯立柱,沈建根,等.毛乌素沙地农田土壤水分动态特征研究[J].中国生态农业学报,2014,22(11):1301-1309.[BAO Han,HOU Lizhu,SHEN Jiangen,et al. Research on soil water dynamics of farmland in Mu Us Sand Land[J]. Chinese Journal of Eco-Agriculture,2014,22(11):1301-1309.]
[8]马建鹏,董建国,汪有科,等.黄土丘陵区枣林地土壤水分时空变化研究[J].中国生态农业学报,2015,23(7):232-232.[MA Jianpeng,DONG Jianguo,WANG Youke,et al. Temporal and spatial variations in soil moisture under jujube forests in the Loess Hilly Region[J]. Chinese Journal of Eco-Agriculture,2015,23(7):232-232.]
[9] YANG L,WEI W,CHEN L D,et al. Response of deep soil moisture to land use and afforestation in the semi-arid Loess Plateau,China[J]. Journal of Hydrology,2012,475(6):111-122.
[10] WESTERN A W,BLOSCHL G,GRAYSON R B. Geostatistical characterization of soil moisture patterns in Tarrawarra catchment[J]. Journal of Hydrology,1998,205(1-2):20-37.
[11] LEGENDRE P,FORTIN M J. Spatial pattern and ecological analysis[J]. Vegetation,1989,80:107-138.
[12]李猛,段文标,陈立新,等.红松阔叶混交林林隙土壤水分分布格局的地统计学分析[J].生态学报,2012,32(5):1396-1402.[LI Meng,DUAN Wenbiao,CHEN Lixin,et al. Geostatistical analysis on spatiotemporal distribution pattern of soil water content of forest gap in Pinus koraiensis dominated broadleaved mixed forest[J]. Acta Ecologica Sinica,2012,32(5):1396-1402.]
[13]王甜,康峰峰,韩海荣,等.山西太岳山小流域土壤水分空间异质性及其影响因子[J].生态学报,2017,37(11):3902-3911.[WANG Tian,KANG Fengfeng,HAN Hairong,et al. Factors influencing spatial heterogeneity of soil moisture content in a small catchment of Mount Taiyue,Shanxi Province[J]. Acta Ecologica Sinica,2017,37(11):3902-3911.]
[14]易小波.西北干旱区土壤含水量时空变化特征及土壤物理性质模拟试验研究[D].杨凌:西北农林科技大学,2017:13-15.[YI Xiaobo. Spatial and temporal variation characteristics of soil moisture content and soil physical properties simulation test in arid area of Northwest China[D]. Yangling:Northwest Agriculture and Forestry University,2017:13-15.]
[15]杨萍萍.永胜县金沙江中游干热河谷地区生态农业发展模式与对策研究[D].成都:成都理工大学,2016:12-13.[YANG Pingping. Study on the development models and countermeasures of eco-agriculture in the dry-hot valley in middle Jinsha River,Yongsheng County[D]. Chengdu:Chengdu University of Technology,2016:12-13.]
[16]韩姣姣,段旭,赵洋毅,等.干热河谷不同土地利用类型坡面土壤水分时空变异[J].水土保持学报,2017,31(2):129-136.[HAN Jiaojiao,DUAN Xu,ZHAO Yangyi,et al. Spatial and temporal variability of soil moisture on sloping lands of different land use types in a dry-hot valley[J]. Journal of Soil and Water Conservation,2017,31(2):129-136.]
[17] ZHAO X,ZHOU D J,ZHOU J Y,et al. Satellite-based studies on large-scale vegetation chanaes in China[J]. Journal of Plant Ecology,2012,54(10):713-728.
[18]陈璟,杨宁.衡阳紫色土丘陵坡地不同植被恢复过程中土壤水文效应[J].中国生态农业学报,2013,21(5):590-597.[CHEN Jing,YANG Ning. Soil hydrological function at different vegetation restoration stages in purple soil slopelands in Hengyang[J]. Chinese Journal of Eco-Agriculture,2013,21(5):590-597.]
[19]原黎明.黑河上游天老池流域土壤水分时空变异的试验研究[D].兰州:兰州大学,2016:15-17.[YUAN Liming. Experimental study on spatial and temporal variation of soil moisture at Tianlaochi Basin in the upper reaches of Heihe River[D].Lanzhou:Lanzhou University,2016:15-17.]
[20]吴维臻.坡面尺度土壤水分空间异质性特征及其与地形因子的关系[D].兰州:兰州大学,2014:14-16.[WU Weizhen. Spatial heterogeneity of soil moisture in slope scale and its relationship with topographic factors[D]. Lanzhou:Lanzhou University,2014:14-16.]
[21]杨泉,赵成章,史丽丽,等.祁连山地甘肃臭草斑块土壤水分的空间自相关分析[J].生态学杂志,2014,33(3):716-722.[YANG Quan,ZHAO Chengzhang,SHI Lili,et al. Spatial autocorrelation analysis on soil moisture of Melica przewalskyi patch in a degraded alpine grassland of Qilian Mountains,Northwest China[J]. Chinese Journal of Ecology,2014,33(3):716-722.]
[22]张露,王益权,石宗琳,等.干旱季节渭北果园土壤水分时空变化特征[J].干旱地区农业研究,2012,30(1):83-89.[ZHANG Lu,WANG Yiquan,SHI Zonglin,et al. Characteristics of spatio-temporal variation of soil moisture in Weibei orchards in dry seasons[J]. Agricultural Research in the Arid Areas,2012,30(1):83-89.]
[23]王俊,刘文兆,胡梦珺.黄土丘陵区小流域土壤水分时空变异[J].应用生态学报,2008,19(6):1241-1247.[WANG Jun,LIU Wenzhao,HU Mengjun. Spatiotemporal variation of soil moisture in a small watershed of loess hilly region[J]. Chinese Journal of Applied Ecology,2008,19(6):1241-1247.]
[24]云雷,毕华兴,田晓玲,等.晋西黄土区林草复合界面雨后土壤水分空间变异规律研究[J].生态环境学报,2010,19(4):938-944.[YUN Lei,BI Huaxing,TIAN Xiaoling,et al. Research on spatial heterogeneity of soil moisture after raining at forest-grassland boundary in the Loess Region of West Shanxi[J]. Ecology and Environmental Sciences,2010,19(4):938-944.]
[25]董彦丽,张富,杨彩红,等.半干旱区微集水系统土壤水分调控效果研究[J].水土保持通报,2013,33(5):35-39.[DONG Yanli,ZHANG Fu,YANG Caihong,et al. Regulation and control effects of soil moisture for micro-catchment water harvesting system in Semiarid Area[J]. Bulletin of Soil and Water Conservation,2013,33(5):35-39.]
[26]王青杵,王改玲,石生新,等.晋北黄土丘陵区不同人工植被对水土流失和土壤水分含量的影响[J].水土保持学报,2012,26(2):71-74.[WANG Qingchu,WANG Gailing,SHI Shengxin,et al. Effect of eifferent artificial vegetation on soil and water loss and soil moisture in Loess Hilly Area in northern Shanxi Province[J].Journal of Soil and Water Conservation,2012,26(2):71-74.]
[27]王安琪,施建成,宫辉力,等.降尺度土壤水分信息与植被生长参量的时空关系[J].农业工程学报,2012,28(增刊1):164-169.[WANG Anqi,SHI Jiancheng,GONG Huili,et al. Space-time analysis on downscaled soil moisture data and parameters of plant growth[J]. Transactions of the Chinese Society of Agricultural Engineering,2012,28(Suppl. 1):164-169.]
[28]赵磊磊,朱清科,聂立水,等.陕北黄土区陡坡土壤水分变异规律研究[J].生态环境学报,2012,21(2):253-259.[ZHAO Leilei,ZHU Qingke,NIE Lishui,et al. Soil moisture variation patterns of steep slope in the loess region in northern Shaanxi Province[J]. Ecology and Environmental Sciences,2012,21(2):253-259.]
[29]费喜亮,张新民,景凌云,等.半干旱黄土区土壤水分垂直分布规律的研究——以甘肃省兰州市孙家岔流域为例[J].土壤学报,2013,50(4):652-656.[FEI Xiliang,ZHANG Xinmin,JING Lingyun,et al. Vertical variability of soil moisture content in semiarid loess region:A case study of Sunjiacha Basin of Lanzhou in Gansu Province[J]. Acta Pedologica Sinica,2013,50(4):652-656.]
[30]姚雪玲,傅伯杰,吕一河.黄土丘陵沟壑区坡面尺度土壤水分空间变异及影响因子[J].生态学报,2012,32(16):4961-4968.[YAO Xueling,FU Bojie,LYU Yihe. Spatial patterns of soil moisture at transect scale in the Loess Plateau of China[J]. Acta Ecologica Sinica,2012,32(16):4961-4968.]
[31]宗路平,角媛梅,李石华,等.哈尼梯田景观水源区土壤水分时空变异性[J].生态学杂志,2015,34(6):1650-1659.[ZONG Luping,JIAO Yuanmei,LI Shihua,et al. Spatial and temporal variability of soil moisture in water source region of Hani terrace landscape[J]. Chinese Journal of Ecology,2015,34(6):1650-1659.]
[32]徐慧芳,宋同清,黄国勤,等.喀斯特峰丛洼地区坡地不同土地利用方式下土壤水分的时空变异特征[J].生态学报,2014,34(18):5311-5319.[XU Huifang,SONG Tongqing,HUANG Guoqin,et al. Spatiotemporal variation of soil moisture under different land use types in a typical karst hill region[J]. Acta Ecologica Sinica,2014,34(18):5311-5319.]
[2] REN Q S,MA P,LI C X,et al. Evaluation of bacterial diversity under different herb vegetation types in the hydro-fluctuation zone of the Three Gorges Reservoir in China[J]. Acta Ecologica Sinica,2016.
[3] FENG W,YANG W B,TANG J N,et al. Deep soil water infiltration and its dynamic characteristics in Chinese Deserts[J]. Journal of Desert Research,2015.
[4] FU Z Y,LI Z X,CAI C F,et al. Soil thickness effect on hydrological and erosion characteristics under sloping lands:A hydropedological perspective[J]. Geoderma,2011,167(167):41-53.
[5]史志华,朱华德,陈佳,等.小流域土壤水分空间异质性及其与环境因子的关系[J].应用生态学报,2012,23(4):889-895.[SHI Zhihua,ZHU Huade,CHEN Jia,et al. Spatial heterogeneity of soil moisture and its relationships with environmental factors at small catchment level[J]. Chinese Journal of Applied Ecology,2012,23(4):889-895.]
[6] YU F,ZHAO Y S. A new semi-empirical model for soil moisture content retrieval by ASAR and TM data in vegetation-covered areas[J]. Science China Earth Sciences,2011,54(12):1955-1964.
[7]包含,侯立柱,沈建根,等.毛乌素沙地农田土壤水分动态特征研究[J].中国生态农业学报,2014,22(11):1301-1309.[BAO Han,HOU Lizhu,SHEN Jiangen,et al. Research on soil water dynamics of farmland in Mu Us Sand Land[J]. Chinese Journal of Eco-Agriculture,2014,22(11):1301-1309.]
[8]马建鹏,董建国,汪有科,等.黄土丘陵区枣林地土壤水分时空变化研究[J].中国生态农业学报,2015,23(7):232-232.[MA Jianpeng,DONG Jianguo,WANG Youke,et al. Temporal and spatial variations in soil moisture under jujube forests in the Loess Hilly Region[J]. Chinese Journal of Eco-Agriculture,2015,23(7):232-232.]
[9] YANG L,WEI W,CHEN L D,et al. Response of deep soil moisture to land use and afforestation in the semi-arid Loess Plateau,China[J]. Journal of Hydrology,2012,475(6):111-122.
[10] WESTERN A W,BLOSCHL G,GRAYSON R B. Geostatistical characterization of soil moisture patterns in Tarrawarra catchment[J]. Journal of Hydrology,1998,205(1-2):20-37.
[11] LEGENDRE P,FORTIN M J. Spatial pattern and ecological analysis[J]. Vegetation,1989,80:107-138.
[12]李猛,段文标,陈立新,等.红松阔叶混交林林隙土壤水分分布格局的地统计学分析[J].生态学报,2012,32(5):1396-1402.[LI Meng,DUAN Wenbiao,CHEN Lixin,et al. Geostatistical analysis on spatiotemporal distribution pattern of soil water content of forest gap in Pinus koraiensis dominated broadleaved mixed forest[J]. Acta Ecologica Sinica,2012,32(5):1396-1402.]
[13]王甜,康峰峰,韩海荣,等.山西太岳山小流域土壤水分空间异质性及其影响因子[J].生态学报,2017,37(11):3902-3911.[WANG Tian,KANG Fengfeng,HAN Hairong,et al. Factors influencing spatial heterogeneity of soil moisture content in a small catchment of Mount Taiyue,Shanxi Province[J]. Acta Ecologica Sinica,2017,37(11):3902-3911.]
[14]易小波.西北干旱区土壤含水量时空变化特征及土壤物理性质模拟试验研究[D].杨凌:西北农林科技大学,2017:13-15.[YI Xiaobo. Spatial and temporal variation characteristics of soil moisture content and soil physical properties simulation test in arid area of Northwest China[D]. Yangling:Northwest Agriculture and Forestry University,2017:13-15.]
[15]杨萍萍.永胜县金沙江中游干热河谷地区生态农业发展模式与对策研究[D].成都:成都理工大学,2016:12-13.[YANG Pingping. Study on the development models and countermeasures of eco-agriculture in the dry-hot valley in middle Jinsha River,Yongsheng County[D]. Chengdu:Chengdu University of Technology,2016:12-13.]
[16]韩姣姣,段旭,赵洋毅,等.干热河谷不同土地利用类型坡面土壤水分时空变异[J].水土保持学报,2017,31(2):129-136.[HAN Jiaojiao,DUAN Xu,ZHAO Yangyi,et al. Spatial and temporal variability of soil moisture on sloping lands of different land use types in a dry-hot valley[J]. Journal of Soil and Water Conservation,2017,31(2):129-136.]
[17] ZHAO X,ZHOU D J,ZHOU J Y,et al. Satellite-based studies on large-scale vegetation chanaes in China[J]. Journal of Plant Ecology,2012,54(10):713-728.
[18]陈璟,杨宁.衡阳紫色土丘陵坡地不同植被恢复过程中土壤水文效应[J].中国生态农业学报,2013,21(5):590-597.[CHEN Jing,YANG Ning. Soil hydrological function at different vegetation restoration stages in purple soil slopelands in Hengyang[J]. Chinese Journal of Eco-Agriculture,2013,21(5):590-597.]
[19]原黎明.黑河上游天老池流域土壤水分时空变异的试验研究[D].兰州:兰州大学,2016:15-17.[YUAN Liming. Experimental study on spatial and temporal variation of soil moisture at Tianlaochi Basin in the upper reaches of Heihe River[D].Lanzhou:Lanzhou University,2016:15-17.]
[20]吴维臻.坡面尺度土壤水分空间异质性特征及其与地形因子的关系[D].兰州:兰州大学,2014:14-16.[WU Weizhen. Spatial heterogeneity of soil moisture in slope scale and its relationship with topographic factors[D]. Lanzhou:Lanzhou University,2014:14-16.]
[21]杨泉,赵成章,史丽丽,等.祁连山地甘肃臭草斑块土壤水分的空间自相关分析[J].生态学杂志,2014,33(3):716-722.[YANG Quan,ZHAO Chengzhang,SHI Lili,et al. Spatial autocorrelation analysis on soil moisture of Melica przewalskyi patch in a degraded alpine grassland of Qilian Mountains,Northwest China[J]. Chinese Journal of Ecology,2014,33(3):716-722.]
[22]张露,王益权,石宗琳,等.干旱季节渭北果园土壤水分时空变化特征[J].干旱地区农业研究,2012,30(1):83-89.[ZHANG Lu,WANG Yiquan,SHI Zonglin,et al. Characteristics of spatio-temporal variation of soil moisture in Weibei orchards in dry seasons[J]. Agricultural Research in the Arid Areas,2012,30(1):83-89.]
[23]王俊,刘文兆,胡梦珺.黄土丘陵区小流域土壤水分时空变异[J].应用生态学报,2008,19(6):1241-1247.[WANG Jun,LIU Wenzhao,HU Mengjun. Spatiotemporal variation of soil moisture in a small watershed of loess hilly region[J]. Chinese Journal of Applied Ecology,2008,19(6):1241-1247.]
[24]云雷,毕华兴,田晓玲,等.晋西黄土区林草复合界面雨后土壤水分空间变异规律研究[J].生态环境学报,2010,19(4):938-944.[YUN Lei,BI Huaxing,TIAN Xiaoling,et al. Research on spatial heterogeneity of soil moisture after raining at forest-grassland boundary in the Loess Region of West Shanxi[J]. Ecology and Environmental Sciences,2010,19(4):938-944.]
[25]董彦丽,张富,杨彩红,等.半干旱区微集水系统土壤水分调控效果研究[J].水土保持通报,2013,33(5):35-39.[DONG Yanli,ZHANG Fu,YANG Caihong,et al. Regulation and control effects of soil moisture for micro-catchment water harvesting system in Semiarid Area[J]. Bulletin of Soil and Water Conservation,2013,33(5):35-39.]
[26]王青杵,王改玲,石生新,等.晋北黄土丘陵区不同人工植被对水土流失和土壤水分含量的影响[J].水土保持学报,2012,26(2):71-74.[WANG Qingchu,WANG Gailing,SHI Shengxin,et al. Effect of eifferent artificial vegetation on soil and water loss and soil moisture in Loess Hilly Area in northern Shanxi Province[J].Journal of Soil and Water Conservation,2012,26(2):71-74.]
[27]王安琪,施建成,宫辉力,等.降尺度土壤水分信息与植被生长参量的时空关系[J].农业工程学报,2012,28(增刊1):164-169.[WANG Anqi,SHI Jiancheng,GONG Huili,et al. Space-time analysis on downscaled soil moisture data and parameters of plant growth[J]. Transactions of the Chinese Society of Agricultural Engineering,2012,28(Suppl. 1):164-169.]
[28]赵磊磊,朱清科,聂立水,等.陕北黄土区陡坡土壤水分变异规律研究[J].生态环境学报,2012,21(2):253-259.[ZHAO Leilei,ZHU Qingke,NIE Lishui,et al. Soil moisture variation patterns of steep slope in the loess region in northern Shaanxi Province[J]. Ecology and Environmental Sciences,2012,21(2):253-259.]
[29]费喜亮,张新民,景凌云,等.半干旱黄土区土壤水分垂直分布规律的研究——以甘肃省兰州市孙家岔流域为例[J].土壤学报,2013,50(4):652-656.[FEI Xiliang,ZHANG Xinmin,JING Lingyun,et al. Vertical variability of soil moisture content in semiarid loess region:A case study of Sunjiacha Basin of Lanzhou in Gansu Province[J]. Acta Pedologica Sinica,2013,50(4):652-656.]
[30]姚雪玲,傅伯杰,吕一河.黄土丘陵沟壑区坡面尺度土壤水分空间变异及影响因子[J].生态学报,2012,32(16):4961-4968.[YAO Xueling,FU Bojie,LYU Yihe. Spatial patterns of soil moisture at transect scale in the Loess Plateau of China[J]. Acta Ecologica Sinica,2012,32(16):4961-4968.]
[31]宗路平,角媛梅,李石华,等.哈尼梯田景观水源区土壤水分时空变异性[J].生态学杂志,2015,34(6):1650-1659.[ZONG Luping,JIAO Yuanmei,LI Shihua,et al. Spatial and temporal variability of soil moisture in water source region of Hani terrace landscape[J]. Chinese Journal of Ecology,2015,34(6):1650-1659.]
[32]徐慧芳,宋同清,黄国勤,等.喀斯特峰丛洼地区坡地不同土地利用方式下土壤水分的时空变异特征[J].生态学报,2014,34(18):5311-5319.[XU Huifang,SONG Tongqing,HUANG Guoqin,et al. Spatiotemporal variation of soil moisture under different land use types in a typical karst hill region[J]. Acta Ecologica Sinica,2014,34(18):5311-5319.]
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |