深圳市5类城市绿地土壤渗透性研究
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摘要
为探明深圳市不同类型绿地土壤渗透性特征,依据CJJ/T85-2017《城市绿地分类标准》,选择G1公园绿地、G2生产绿地、G3防护绿地、G4附属绿地和G5其他绿地进行土壤渗透性测定和定量分析。结果表明:(1)各绿地土壤水分渗透率依次为:生产绿地>防护绿地>其他绿地>公园绿地>附属绿地,3项渗透特征值为:初渗率>平均渗透率>稳渗率,入渗率随着土壤深度增加呈减小趋势;(2)经考氏经验公式对水分入渗模型拟合,各拟合模型的相关系数R2≥0.748 8;(3)对土壤渗透性与主要土壤因子进行相关性分析,发现初渗率、平均渗透率和稳渗率与土壤容重呈极显著负相关,与土壤总孔隙度和非毛管孔隙度呈极显著正相关,平均渗透率与毛管孔隙度呈显著负相关,其余比对虽有相关关系,但均未达到显著水平。
The soil permeability of 5 types of greenland in Shenzhen was studied according to CJJ/T85-2017 Classification Criterion for urban greenlands.5 different locations were selected as follows:G1 park greenland,G2 production greenland,G3 protective greenland,G4 suburban greenland,and G5 other greenland.The results showed that the order of soil moisture permeability was G2>G3>G5>G1>G4.And the order of 3 penetration eigen values were infiltration rate> average permeability> stable infiltration rate and the infiltration rate decreases with the increase of soil depth.Moreover,the water infiltration model was fitted to Kostiakov's model and the correlation coefficient R2 of each model was≥0.748 8 in general.Correlation analysis of soil permeability showed that the main different soil factors such as the initial infiltration rate,average permeability,and stable infiltration rate were significantly negatively correlated with soil bulk density while the fore-mentioned factors were significantly positively correlated to the total soil and non-capillary porosity and the average permeability was significantly negatively correlated with capillary porosity.The rest parameters showed correlation at certain degree,but not significant.
The soil permeability of 5 types of greenland in Shenzhen was studied according to CJJ/T85-2017 Classification Criterion for urban greenlands.5 different locations were selected as follows:G1 park greenland,G2 production greenland,G3 protective greenland,G4 suburban greenland,and G5 other greenland.The results showed that the order of soil moisture permeability was G2>G3>G5>G1>G4.And the order of 3 penetration eigen values were infiltration rate> average permeability> stable infiltration rate and the infiltration rate decreases with the increase of soil depth.Moreover,the water infiltration model was fitted to Kostiakov's model and the correlation coefficient R2 of each model was≥0.748 8 in general.Correlation analysis of soil permeability showed that the main different soil factors such as the initial infiltration rate,average permeability,and stable infiltration rate were significantly negatively correlated with soil bulk density while the fore-mentioned factors were significantly positively correlated to the total soil and non-capillary porosity and the average permeability was significantly negatively correlated with capillary porosity.The rest parameters showed correlation at certain degree,but not significant.
引文
[1]王艳红,宋维峰,李财金.不同竹林地土壤水分入渗研究[J].水土保持研究,2009,16(2):165-168.
[2]刘道平,陈三雄,张金池,等.浙江安吉主要林地类型土壤渗透性[J].应用生态学报,2007,18(3):493-498.
[3]王景燕,龚伟,胡庭兴,等.川南天然常绿阔叶林人工更新后的土壤水源涵养功能[J].浙江林学院学报,2007,24(5):569-574.
[4]刘艇,李维义,王继红,等.侵蚀与非侵蚀黑土入渗性能差异性研究[J].水土保持学报,2010,24(2):83-86.
[5]霍小鹏,李贤伟,张健,等.川西亚高山人工针叶林枯落物持水与土壤渗透性能[J].长江流域资源与环境,2010,19(5):540-546.
[6]马文梅,马云飞,张兴昌.砒砂岩区原状和扰动土壤水分入渗过程[J].水土保持学报,2018,32(2):128-132.
[7]刘广路,范少辉,漆良华,等.不同类型毛竹林土壤渗透性研究[J].水土保持学报,2008,22(6):44-47.
[8]谢丽纯,陈建耀,付丛生,等.华南滨海小流域降雨入渗对地下水的补给分析[J].生态环境学报,2011(20):8-9.
[9]林代杰,郑子成,张锡洲,等.不同土地利用方式下土壤入渗特征及其影响因素[J].水土保持学报,2010,24(1):33-36.
[10]李义,程本军.基于土壤入渗模型的研究[J].黑龙江水利科技,2013(3):41,13-14.
[11]杨永辉,赵世伟,雷廷武,等.耕作对土壤入渗性能的影响[J].生态学报,2006,26(5):1624-1630.
[12]杜阿朋,何常清,管伟,等.六盘山叠叠沟小流域土壤稳渗速率及其影响因子[J].林业科学,2011,20(8-9):1259-1266.
[13]张雅楠;黄兴法;毛丽丽,等.土壤入渗性能自动测量系统原理与应用研究[J].农业工程学报,2007,23(4):99-103.
[14]Philip J R.Theory of infiltration[M].Advance in Hydroscience,1969:216-296.
[15]Hillel D.soil and water-physical principles and process[M].New York:Academic Press,1977.
[16]Wang G L,Liu G B.Effect of stip a bungeana communities on soil infiltration in soil profile in Loess Hilly Region[J].Journal of Soil and Water Conservation,2009,23(3):227-231.
[17]Li X Z,Fan G S.Influence of organic matter content on infiltration capacity and parameter in field soils[J].Transactions of the CSAE,2006,22(3):188-190.
[18]古炎坤.生态资源可持续发展理论与实践:广州市白云山国家重点风景名胜区[M].广州:中国林业出版社,2005:160-174.
[19]国家林业局.中华人民共和国林业行业标准:森林土壤分析方法[M].北京:中国标准出版社,1999:22-24,32-33.
[20]CJJ/T85-2017.城市绿地分类标准[R].北京:中国建筑工业出版社,2017.
[21]刘凯,王磊,宋乃平,等.毛乌素沙地南缘不同林龄人工柠条林土壤渗透性研究[J].干旱区资源与环境,2013,27(5):89-94.
[22]马田田,柯浩成,李占斌,等.次降雨事件下雨养区典型小流域土壤水分运移规律[J].水土保持学报,2018,32(2):80-86.
[23]刘目兴,杜文正,张海林,等.三峡库区不同林型土壤的入渗能力研究[J].长江流域资源与环境,2013,23(3):299-305.
[24]王猛,袁福锦,吴文荣,等.封育对滇西北亚高山草甸群落及土壤的影响[J].草原与草坪,2017,37(2):69-73.
[25]李建兴,何丙辉,谌芸.不同护坡草本植物的根系特征及对土壤渗透性的影响[J].生态学报,2013,33(5):1535-1544.
[26]喻明美,谢正生.广州市白云山五种森林类型的土壤渗透性研究[J].水土保持研究,2011,18(1):153-156.
[27]刘锦晖,刘学录.嘉峪关城市公园绿地的空间分布与服务范围分析[J].草原与草坪,2017,37(5):41-46.
[28]李卓,吴普特,冯浩,等.容重对土壤水分入渗能力影响模拟试验[J].农业工程学报,2009,25(6):40-45.
[29]范少辉,刘广路,漆良华,等.闽西北不同经营时间毛竹林土壤渗透性研究[J].水土保持学报,2010,24(1):24-28.
[30]赵洋毅,段旭.滇东石漠化地区不同植被模式土壤渗透性研究[J].水土保持研究,2014,21(1):45-49
[31]李雪转,樊贵盛.土壤有机质含量对土壤入渗能力及参数影响的试验研究[J].农业工程学报,2006,22(3):188-190.
[32]杨满元,杨宁,陈志阳,等.衡阳紫色土丘陵坡地不同恢复阶段土壤渗透性研究与评价[J].湖南环境生物职业技术学院学报,2013,19(1):5-9.
[2]刘道平,陈三雄,张金池,等.浙江安吉主要林地类型土壤渗透性[J].应用生态学报,2007,18(3):493-498.
[3]王景燕,龚伟,胡庭兴,等.川南天然常绿阔叶林人工更新后的土壤水源涵养功能[J].浙江林学院学报,2007,24(5):569-574.
[4]刘艇,李维义,王继红,等.侵蚀与非侵蚀黑土入渗性能差异性研究[J].水土保持学报,2010,24(2):83-86.
[5]霍小鹏,李贤伟,张健,等.川西亚高山人工针叶林枯落物持水与土壤渗透性能[J].长江流域资源与环境,2010,19(5):540-546.
[6]马文梅,马云飞,张兴昌.砒砂岩区原状和扰动土壤水分入渗过程[J].水土保持学报,2018,32(2):128-132.
[7]刘广路,范少辉,漆良华,等.不同类型毛竹林土壤渗透性研究[J].水土保持学报,2008,22(6):44-47.
[8]谢丽纯,陈建耀,付丛生,等.华南滨海小流域降雨入渗对地下水的补给分析[J].生态环境学报,2011(20):8-9.
[9]林代杰,郑子成,张锡洲,等.不同土地利用方式下土壤入渗特征及其影响因素[J].水土保持学报,2010,24(1):33-36.
[10]李义,程本军.基于土壤入渗模型的研究[J].黑龙江水利科技,2013(3):41,13-14.
[11]杨永辉,赵世伟,雷廷武,等.耕作对土壤入渗性能的影响[J].生态学报,2006,26(5):1624-1630.
[12]杜阿朋,何常清,管伟,等.六盘山叠叠沟小流域土壤稳渗速率及其影响因子[J].林业科学,2011,20(8-9):1259-1266.
[13]张雅楠;黄兴法;毛丽丽,等.土壤入渗性能自动测量系统原理与应用研究[J].农业工程学报,2007,23(4):99-103.
[14]Philip J R.Theory of infiltration[M].Advance in Hydroscience,1969:216-296.
[15]Hillel D.soil and water-physical principles and process[M].New York:Academic Press,1977.
[16]Wang G L,Liu G B.Effect of stip a bungeana communities on soil infiltration in soil profile in Loess Hilly Region[J].Journal of Soil and Water Conservation,2009,23(3):227-231.
[17]Li X Z,Fan G S.Influence of organic matter content on infiltration capacity and parameter in field soils[J].Transactions of the CSAE,2006,22(3):188-190.
[18]古炎坤.生态资源可持续发展理论与实践:广州市白云山国家重点风景名胜区[M].广州:中国林业出版社,2005:160-174.
[19]国家林业局.中华人民共和国林业行业标准:森林土壤分析方法[M].北京:中国标准出版社,1999:22-24,32-33.
[20]CJJ/T85-2017.城市绿地分类标准[R].北京:中国建筑工业出版社,2017.
[21]刘凯,王磊,宋乃平,等.毛乌素沙地南缘不同林龄人工柠条林土壤渗透性研究[J].干旱区资源与环境,2013,27(5):89-94.
[22]马田田,柯浩成,李占斌,等.次降雨事件下雨养区典型小流域土壤水分运移规律[J].水土保持学报,2018,32(2):80-86.
[23]刘目兴,杜文正,张海林,等.三峡库区不同林型土壤的入渗能力研究[J].长江流域资源与环境,2013,23(3):299-305.
[24]王猛,袁福锦,吴文荣,等.封育对滇西北亚高山草甸群落及土壤的影响[J].草原与草坪,2017,37(2):69-73.
[25]李建兴,何丙辉,谌芸.不同护坡草本植物的根系特征及对土壤渗透性的影响[J].生态学报,2013,33(5):1535-1544.
[26]喻明美,谢正生.广州市白云山五种森林类型的土壤渗透性研究[J].水土保持研究,2011,18(1):153-156.
[27]刘锦晖,刘学录.嘉峪关城市公园绿地的空间分布与服务范围分析[J].草原与草坪,2017,37(5):41-46.
[28]李卓,吴普特,冯浩,等.容重对土壤水分入渗能力影响模拟试验[J].农业工程学报,2009,25(6):40-45.
[29]范少辉,刘广路,漆良华,等.闽西北不同经营时间毛竹林土壤渗透性研究[J].水土保持学报,2010,24(1):24-28.
[30]赵洋毅,段旭.滇东石漠化地区不同植被模式土壤渗透性研究[J].水土保持研究,2014,21(1):45-49
[31]李雪转,樊贵盛.土壤有机质含量对土壤入渗能力及参数影响的试验研究[J].农业工程学报,2006,22(3):188-190.
[32]杨满元,杨宁,陈志阳,等.衡阳紫色土丘陵坡地不同恢复阶段土壤渗透性研究与评价[J].湖南环境生物职业技术学院学报,2013,19(1):5-9.
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