摘要
准格尔丘陵区位于鄂尔多斯高原最西端 ,是黄河中游水土流失治理、生态环境建设的重点区域。2 0 0 1年 8月中下旬 ,在自然条件下 ,对准格尔丘陵区主要天然优势植物群落百里香群落、沙打旺人工草地和沙棘灌木林的蒸腾耗水特征应用 L I- 1 6 0 0稳态气孔计同时进行野外测定。结果表明 :百里香和沙棘的蒸腾速率都无午休现象 ,百里香蒸腾速率峰值出现在下午 1 6 :0 0 ;沙棘在 1 2 :0 0~ 1 6 :0 0时间段内都呈较高的蒸腾速率 ,两者都为单峰型。达乌里胡枝子、糙隐子草和沙打旺的蒸腾速率日变化曲线则呈不明显的双峰型。以上 5种植物日蒸腾速率平均值从大到小的排列顺序为百里香 >达乌里胡枝子 >沙棘 >糙隐子草 >沙打旺。在连续 3年干旱和人为原因致使沙棘灌木林长势不好的情况下 ,单位面积 (1 m× 1 m )沙打旺人工草地日蒸腾累计失水量最大 ,为 75 70 .5 g,百里香群落居中 ,为 2 0 71 .4 g,沙棘灌木林最小 ,为 1 1 6 9.
The Zhungeer hilly region is located in the west part of the Ordos Plateau, Inner Mongolia, it is a key region for soil erosion control and eco environment restoration in the middle reach of Yellow River. On 20 August 2001, the transpiration characteristics of Thymus serpyllum community, Astragalia adsurgens cv. artificial grassland and Hippophae rhamnoides shrubs forest land were measured under natural conditions by using a portable LI 600 stable stomatal. The results indicated that transpiration rate of Thymus serpyllum and Hippophae rhamnoides had no noon expression, was single peak pattern. For Thymus serpyllum, the highest value appeared in 16:00, for Hippophae rhamnoides, from 12:100~16:00, the rate was all higher. However, transpiration rate of Lespedeza davurica, Cleistogenes squarrosa and Astragalia adsurgens cv. were bimodal pattern. The order of mean of transpiration rate in one day is Thymus serpyllum>Lespedeza davurica>Hippophae rhamnoides>Cleistogenes squarrosa>Astragalia adsurgens cv.. In condition, weather was dry for continuous three years, and some other reasons, water consumption by transpiration of Astragalia adsurgens cv. artificial grassland was biggest, was 7 570.5 g/m 2,Thymus serpyllum community was middle,is 2 071.4 g/m 2, Hippophae rhamnoides shrub forest land was smallest, was 1 169.8 g/m 2.
出处
《水土保持学报》
CSCD
北大核心
2002年第2期96-98,102,共4页
Journal of Soil and Water Conservation
基金
国家重点基础研究发展规划项目 ( G2 0 0 0 0 1 86 0 4)资助
关键词
准格尔丘陵区
植物群落
人工草地
灌木林地
水分生态特征
Thymus serpyllum community
Astragalia adsurgens cv. artificial grassland
Astragalia adsurgens cv. shrub forest land
transpiration rate
water ecology