Moisture content change and characteristic, distribution, formation reason of dried earth layer under artificial forest land and lawn ranging 0~6m depth in Guanzhong Plain were studied in this article by drying-weight method.The aim of the research is to verify the distribution scope of dried earth layer in the south of the Loess Plateau and the reason of it, and to provide scientific basis for the prevention and control of dried earth layer. Experiment results show that the average earth moisture content is 8.4% between 2 and 4m of 10 age apple trees, the average earth moisture content is 9.0% between 2 and 4m of 12 age phoenix trees in Xianyang. The average earth moisture content is between 9.3% and 9.5% between 1.8~3.6m of 12 age phoenix and poplar trees in Lantian. The average earth moisture content is 9.2% between 2 and 3.5m of 15 age apple trees in Wujiafen, and there is formation of dried earth layer between 2 and 3.5m. There is obvious formation of chronic dried earth layer in artificial forest land at Xiekou of Lintong and Weiqu of Chang'an.The average earth moisture content is more than 12% below 4m of the middle age artificial forest land, which indicates that the dried earth layer doesn't extend to the layer below 4m.The average earth moisture content is more than 12% below 2m of 6 age and 4 age apple trees land, and there is no formation of dried earth layer. According to the computation of CaCO3 migration depth model, under 600mm annual precipitation condition in Guanzhong Plain, the migration depth of gravity water is less than 4m, which indicates that the dried earth layer in this area is chronic. The changes of the moisture content of the artificial forest land show that the dried earth layer is distributed extensively on the Loess Plateau, and the south boundary of it has reached the northern foot of the Qinling Mountains.In Northwest China, where annual precipitation is less than 600mm, the dried earth layer in the artificial forest land is a universal natural phenomenon. The formation reason of the dried earth layer is that the gravity-capillary zone depth, which is determined by precipitation, is obviously smaller than 2 m.The direct action of water factor of dried earth layer is that the buried depth of the zone is small and the water movement velocity is slow, while the high water consumption tree species is the vegetation factor of it. It is clearly shown that the depth of the gravity water and the capillary water in Guanzhong Plain is the main natural factor for the formation of the dried earth layers. Whether the artificial forest or natural forest, the dried layers generally develop in the middle age forest land. The formation of the dried layer doesn't mean that the forests can not develop in this area, but they cannot develop well.Trees can be planted in areas where dried earth layer developed poorly, but they are not suitable to be planted in areas where dried earth layer developed intensely.
ZHAO Jing-bo, SUN Gui-zhen, YUE Ying-li, CHEN Bao-qun
. Research of dried earth layer and its formation in the artificial forest land of Guanzhong Plain[J]. GEOGRAPHICAL RESEARCH, 2007
, 26(4)
: 763
-772
.
DOI: 10.11821/yj2007040013
[1] 李玉山.黄土区土壤水分循环特征及其对陆地水分循环的影响.生态学报,1983,3(2):91~101.
[2] 王志强,刘宝元,王晓兰.黄土高原半干旱区天然锦鸡儿灌丛对土壤水分的影响.地理研究,2005,24(1):113~120.
[3] 侯庆春,黄旭,韩仕峰,等.黄土高原地区小老树成因及其改造途径的研究.水土保持学报,1991,5(2):76~83.
[4] 杨文治. 黄土高原土壤水资源与植树造林. 自然资源学报,2001,16(5):433~438.
[5] 黄明斌,杨新良,李玉山,等.黄土区渭北旱塬苹果基地对区域水循环的影响.地理学报,2001,56(1):7~13.
[6] 赵景波,侯甬坚,黄春长.陕北黄土高原人工林下土壤干化原因与防治.中国沙漠,2003,23(6):612~615.
[7] 王力,邵明安,张青峰. 陕北黄土高原土壤干层的分布和分异特征. 应用生态学报,2004,15(3):436~442.
[8] 刘增文,王佑民.人工油松林蒸腾耗水及林地水分动态特征的研究.水土保持通报,1990,10(6):78~84.
[9] 徐宗学, 张楠.黄河流域近50年降水变化趋势分析.地理研究,2006,25(1):27~34.
[10] 陈云明,侯喜禄,刘文兆.黄土丘陵半干旱区不同类型植被水保生态效益研究.水土保持学报,2000,14(3):57~62.
[11] Yuin E. An infiltration model to predict suction changes in the soil profile. Water Resource Research, 1998,34 (7):1617~1622.
[12] Rapp I. Evaporation and crust imperdance role in seeding emergence. Soil Science, 2000,165(4):354~364.
[13] Caims J, Audebent A, Towend J,et al.Effect of mechanical impedance on root growth of two rice varieties under field drought stress.Plant and Soil,2004,267(1-2):309~318.
[14] 付明胜,钱卫东,牛萍,等.连续干旱对土壤干层深度及植物生存的影响.干旱区研究,2002,19(2):71~74.
[15] 杨文治,邵明安.黄土高原土壤水分研究.北京:科学出版社,2000.86~114.
[16] 王志强,刘宝元,路炳军.黄土高原半干旱区土壤干层水分恢复研究.生态学报,2003,23(9):944~1950.
[17] 张海,王延平,高鹏程,等.黄土高原坡地土壤干层形成机理及补水途径研究.水土保持学报,2003,17(3):162~164.
[18] 王力,邵明安,侯庆春.土壤量化指标初探.水土保持学报,2000,14(4):87~ 90.
[19] 赵景波.淀积理论与黄土高原环境演变.北京:科学出版社,2002.165~178.
[20] 赵景波.黄土中古土壤CaCO3淀积层与大气降水入渗形式研究.地理科学,1995,15(4):344~350.
[21] 赵景波.陕西黄土高原500kaBP的古土壤与气候带迁移.地理学报,2001,56(3):323~331.
[22] 李天杰,王芸,郑应顺.土壤地理学.北京:高等教育出版社,1983.49~53.