YI Yan,YI Yan-li.Study on the Feature of Acidity Change in Brown Soils of Changtu County[J].HEILONGJIANG AGRICULTURAL SCIENCES,2011,(09):25-29.
昌图县耕地棕壤酸度变化特征的初步研究
- Title:
- Study on the Feature of Acidity Change in Brown Soils of Changtu County
- 文章编号:
- 1002-2767(2011)09-0025-05
- Keywords:
- cultivated brown soil; soil acidity; distribution characteristic; change trend; correlation
- 分类号:
- S153.4
- 文献标志码:
- A
- 摘要:
- 昌图县位于辽宁省铁岭市北部,是辽宁省的产粮大县之一。通过对大田调查采样与室内分析相结合的方法,研究了昌图县耕地土壤酸度变化特征。结果表明:昌图县耕地土壤类型以棕壤为主,此外还有少量的风沙土和草甸土。在3 750个3种类型土壤土样中,pH<5.0(强酸性)和pH 5.0~6.5(酸性)的土样占总调查土样的75.68%。中性土样占16.56%;其中棕壤酸化程度最大,pH<5.0(强酸性)和pH 5.0~6.5(酸性)的土样分别占总调查土样的1.17%、87.28%。与第二次土壤普查相比,各乡镇土壤pH均有所下降,其下降值为0.16~1.43个单位。实验数据分析得出:土壤pH与土壤阳离子交换量和盐基饱和度呈正相关关系;与土壤交换性酸(交换性H+和交换性Al3+)呈负相关关系。
- Abstract:
- Changtu county locates in the north of Tieling.It is one of the major grain-producing counties in Liaoning province.Using the method of combining the field investigation and analysis indoor,the feature of acidity change in soils of Changtu county was studied.The results showed that besides a small amount of sand soil and meadows soil,soils of Changtu were mainly brown soil.The proportion of the three types of soil which pH<5.0(strongly acidic) and pH 5.0~6.5(acid) accounted for 75.68% of the 3 750 survey soil samples,the neutral soil accounted for 16.56%.Brown soil’s acidification degree was the largest.The soil samples of the pH<5.0(strongly acidic) and pH 5.0~6.5(acid) accounted for 1.17% and 87.28%,respectively.Compared with the second soil census,the soil pH of the towns all decline between 0.16~0.13.The results showed that the soil pH had positive correlations with CEC and BS and negative correlations with exchanged acid(exchanged H+and exchanged Al3+).
参考文献/References:
[1]Gr
é
gory Lesturgez a,c.Soil acidi cation without pH drop under intensive cropping systems in Northeast Thailand[J].Agriculture,Ecosystems and Environment,2006,114:239
-
248.
[2]Mihaila V,Hera C .Long term agricultural experiments in eastern Europe [J].Long-term Experiments in Agricultural and Ecological Science,1993(2):220-227. [3]王志刚,赵永存.近20年来江苏省土壤pH时空变化及其驱动力[J].生态学报,2008,28(2):721-727. [4]Ulrika Jonsson,Ulrika Rosengren,Gunnar Thelin,et al.Acidification-induced chemical changes in coniferous forest soils in southern Sweden 1988-1999[J].Environmental Pollution, 2003,123:75-83. [5]Guo J H,Liu X J,Zhang Y,et al.Significant Acidification in Major Chinese Croplands[J].China Science,2010,2(18):1008-1010. [6]依艳丽,郭琳琳,丁文博,等.沈阳地区典型耕地棕壤养分状况及变化趋势的分析[J].沈阳农业大学学报,2009,40(2):178-182. [7]Cregan P D,Scott B J .Soil acidification an agricultural and environmental problem[M]// Pratley J E,Roberts on A.Agriculture and the Environmental Imperative.Melbourne: CSIRO Publishing,1998:98-128. [8]Hans van Calstera,Lander Baeten.Martin hermy a management driven changes(1967-2005) in soil acidity and the understorey plant community following conversion of a coppice-with-standards forest[J].Forest Ecology and Management,2007(241):258-271. [9]李贤胜,杨平.皖南山区土壤酸化趋势研究[J].土壤,2008,40(4):676-579. [10]〖ZK(#〗朱本岳.菜地土壤酸化原因及其对番茄生产的影响[J].浙江农业大学学报,1989,15(3):273-277. [11]张建华,杨发荣.大理市蔬菜地土壤酸化的原因与调控措施[J].云南农业科技,2004(2):4-6. [12]贾振文,依艳丽.辽宁省昌图县典型耕地棕壤有效态微量元素含量评价[J].安徽农业科学,2009,37(16):7604-7606. [13]陈洪斌,王丽,丁福成.辽宁省耕地土壤1979~1999年土壤养分肥力的变化[J].土壤通报,2003,34(4):271-274. [14]路钰.辽宁省耕地土壤养分调查结果报告[J].杂粮作物,2004,24(3):174-175. [15]贺中科,许讫.铁岭市土壤养分现状与施肥建议[J].土壤肥料,2000(3):195-198. [16]鲍士旦.土壤农化分析[M].北京:中国农业出版社,2000. [17]黄昌勇.土壤学[M].北京:中国农业出版社,2000. [18]熊毅, 李庆逵. 中国土壤[M]. 2版. 北京:科学出版社,1990. [19]魏孝荣,邵明安.黄土高原小流域土壤pH、阳离子交换量和有机质分布特征[J].应用生态学报,2009,20(11):2710-2715. [20]罗淑华,曾跃辉.茶园土壤阳离子交换量研究[J].中国茶叶,1989(5):15-17. [21]孔晓玲,季国亮.我国南方土壤的酸度与交换性氢铝的关系[J].土壤通报,1922,23(5):203-204. [22]刘世全, 张宗锦, 王昌全, 等.西藏酸性土壤的酸度特征[J].土壤学报,2005,42(2):211-218.
备注/Memo
第一作者简介:依妍(1985-),女,辽宁省沈阳市人,在读硕士,从事土壤酸化方面研究。E-mail:woshigege_@126.com.