1. 山东农业大学林学院,山东,泰安,271018
2. 滨州学院山东省黄河三角洲生态环境重点实验室,山东,滨州,256603
3. 潍坊科技学院, 山东寿光,262700
纸质出版:2014
移动端阅览
魏晓明, 夏江宝, 孔雪华, 等. 不同植被类型对黄河三角洲贝壳堤土壤水文功能的影响[J]. 水土保持通报, 2014,33(4):28-32.
WEI Xiao-ming, XIA Jiang-bao, KONG Xue-hua, et al. Effect of Different Vegetation Types on Soil Hydrological Function at Shell Ridge in Yellow Delta[J]. Bulletin of Soiland Water Conservation, 2014, 33(4): 28-32.
魏晓明, 夏江宝, 孔雪华, 等. 不同植被类型对黄河三角洲贝壳堤土壤水文功能的影响[J]. 水土保持通报, 2014,33(4):28-32. DOI: 10.13961/j.cnki.stbctb.2014.04.020.
WEI Xiao-ming, XIA Jiang-bao, KONG Xue-hua, et al. Effect of Different Vegetation Types on Soil Hydrological Function at Shell Ridge in Yellow Delta[J]. Bulletin of Soiland Water Conservation, 2014, 33(4): 28-32. DOI: 10.13961/j.cnki.stbctb.2014.04.020.
以滩涂裸地为对照
对黄河三角洲贝壳堤向海侧的盐生灌草、滩脊地带的旱生灌草及向陆侧的盐生草3种植被类型的土壤水文功能进行了研究。结果表明
与裸地相比
贝壳堤生境条件下的盐生灌草、旱生灌草及盐生草3种植被类型土壤容重降低了8.5%~20.8%
总孔隙度增加了17.1%~46.1%。滩脊地带的旱生灌草改善土壤孔隙状况效果最好
向陆侧的盐生草最差。3种植被类型具有一定的压碱抑盐效应
降盐碱功能表现为滩脊地带的旱生灌草最好
其次为向海侧的盐生灌草
而向陆侧盐生草最差。不同被覆地类土壤渗透性能大小表现为:向陆侧盐生草 < 滩脊地带旱生灌草 < 向海侧盐生灌草 < 裸地。0-40 cm土层的土壤饱和贮水量和毛管贮水量表现为:滩脊地带旱生灌草 > 向海侧盐生灌草 > 向陆侧盐生草。在垂直层次上
贝壳堤不同植被类型改良盐碱、土壤孔隙状况及贮水性能均表现为0-20 cm优于20-40 cm土层。研究表明
贝壳堤滩脊地带旱生灌草植被的土壤贮蓄水分及降盐改土能力最优
其次为向海侧的盐生灌草
向陆侧的盐生草较差。
Compared with bare land
soil hydrological characteristics of three kinds of saline bringing
xerophytic bringing and saline herbaceous were researched in shell ridge island of the Yellow River Delta. Results indicated that compared with bare land
the soil bulk density of three vegetation types decreased by 8.5%~20.8%
soil total porosity increased by 17.1%~46.1%
the effect of xerophytic bringing vegetation in beach ridge zone was the best
the effect of saline herbaceous vegetation close to landside was the worst. The sequence of the soil permeability characteristics of different vegetation types was in the following increasing order: saline herbaceous vegetation close to landside < xerophytic bringing vegetation in beach ridge zone < saline bringing vegetation close to the seaside < bare land. The sequence of the soil saturated water and capillary water of the soil layer in 0-40 cm was in the following decreasing order: xerophytic bringing vegetation in beach ridge zone > saline bringing vegetation close to the seaside > saline herbaceous vegetation close to landside. The soil water storage performance and improved effect of the soil layer in 0-20 cm were better than that in 20-40 cm. The ability of soil water savings
salt reducing and soil improving of xerophytic bringing vegetation in beach ridge zone was the best
that of saline herbaceous vegetation close to landside was the worst.
田家怡,夏江宝,孙景宽,等.黄河三角洲贝壳堤岛生态保护与恢复技术[M].北京:化学工业出版社,2011.
赵艳云,田家怡,孙景宽,等.滨州北部贝沙堤生物多样性现状及影响因素的研究[J].水土保持研究,2010,17(2):136-140.
赵艳云,胡相明,刘京涛.贝壳堤地区微生物分布特征及其与植被分布的关系[J].水土保持通报,2012,32(2):267-270.
夏江宝,孔雪华,陆兆华,等.滨海湿地不同密度柽柳林土壤调蓄水功能[J].水科学进展,2012,23(5):628-634.
徐丽宏,王彦辉,熊伟,等.六盘山典型植被类型土壤水文生态功能研究[J].林业科学研究,2012,25(4):456-463.
陈波,剪文灏,吕发,等.冀北山地蒙古栎天然林土壤物理性质及水源涵养功能研究[J].水土保持通报,2013,33(2):83-86.
刘小林,郑子龙,蔺岩雄,等.甘肃小陇山林区主要林分类型土壤水分物理性质研究[J].西北林学院学报,2013,28(1):7-11.
周玮,朱军,吴鹏,等.杠寨小流域不同植被下土壤水分物理特性的研究[J].中南林业科技大学学报,2012,32(5):92-96.
Liu Xia, Zhang Guangcan, Gary C H. Fractal features of soil particle-size distribution as affected by plant communities in the forested region of Mountain Yimeng, China[J]. Geoderma, 2009,154(1/2):123-130.
李建兴,何丙辉,梅雪梅,等.紫色土区坡耕地不同种植模式对土壤渗透性的影响[J].应用生态学报,2013,24(3):725-731.
王贵霞,李传荣,许景伟,等.沙质海岸5种植被类型土壤物理性状及其水源涵养功能[J].水土保持学报,2005,19(2):142-146.
齐清,李传荣,许景伟,等.沙质海岸不同植被类型土壤水源涵养功能的研究[J].水土保持学报,2005,19(6):102-105.
夏江宝,刘庆,谢文军,等.废水灌溉对芦苇地土壤水文特征的影响[J].农业工程学报,2009,25(12):63-68.
王晓芳,夏江宝.黄河三角洲引黄灌区不同植被类型的降盐改土功能[J].水土保持学报,2012,26(3):141-144.
Murray C D, Buttle J M.Infiltration and soil water mixing on forested and harvested slopes during spring snowmelt, Turkey lakes watershed, central Ontario[J]. Journal Hydrology, 2005, 306(1/4):1-20.
Rosa J D, Cooper M, Darboux F, et al. Soil roughness evolution in different tillage systems under simulated rainfall using a semivariogram-based index[J]. Soil and Tillage Research, 2012,124(8):226-232.
0
浏览量
1331
下载量
0
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621