摘要
[目的]研究黄土丘陵区植被恢复过程中土壤水分、可溶性碳氮的变化特征。[方法]选择刺槐（乔木）、柠条（灌木）、撂荒地（草地）3种退耕植被为研究对象，以坡耕地为对照，研究不同退耕植被下土壤水分、可溶性碳氮的季节和垂直分布。[结果]土壤水分、可溶性碳氮均受季节变化的影响，其中土壤水分表现为先降低后增加的趋势，可溶性碳氮的趋势相反；此外，与耕地相比，3种退耕植被土壤水分、可溶性碳氮均有较大的提高；随着土层的加深，土壤水分在表层（0～30 cm）整体表现为撂荒地较林地低，而30～200 cm土层，表现为撂荒地大于林地，深层土壤水分变化不显著。可溶性碳氮在0～30 cm土层也表现为随着土层的增加而递减趋势，且显著受土层变化的影响（P＜0．05）。另外，土壤水分、可溶性碳氮存在着显著相关性（P＜0．05）。[结论]该研究阐明了黄土丘陵区典型退耕植被的土壤水分、可溶性碳氮的动态变化规律，为进一步分析和评价黄土丘陵区土壤养分状况提供科学依据。
Abstract
Objective] In order to study the changes of the soil water content ( SWC) , dissolved organic carbon and nitrogen ( DOC/DON) during the vegetation restoration on the Loess Hilly Region of China.[ Method] Robinia pseudoacacia L., Caragana korshinskii Kom, and a-bandoned land, were selected, with slope farmland as control.The seasonal and vertical distribution of SWC and DOC/DON under different kinds of vegetation were studied.[ Result] The results showed that SWC, DOC, and DON were affected by seasonal variations; the SWC showed the increasing after decreasing trend, while both the DOC and DON showed the contrary.Additionally, compared to the farmland, af-forestation greatly increased the SWC, DOC and DON.Furthermore, SWC showed the trend of abandoned land<R.pseudoacacia (CK) at the depth of 0-30 cm; but in the deep soil (30-200 cm), the SWC in forest (R.pseudoacacia and CK) was higher than that in abandoned land.Moreover, significant decrease in DOC and DON were observed from the depth of 0-10 cm to 20-30 cm and significant correlation be-tween SWC and DOC/DON were also showed (P<0.05).[Conclusion] Therefore, this study illustrated the dynamic changes of SWC and dissolved organic carbon/nitrogen in typical vegetation restoration of loess hilly region, which provided a scientific basis for further analyzing and evaluating the soil nutrients status on the Loess Hilly Region of China .
基金项目
国家林业部公益性行业科研专项(201304312)
国家自然科学基金(41301601)
国家科技期刊平台
NSTL
万方数据