Cheng Jimin, Wan Hui'e, Wang Jing
Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Northwest Sci-Tech University of Agriculture and Forestry, Yangling 712100, China.
Ying Yong Sheng Tai Xue Bao. 2005 Mar;16(3):435-8.
This paper studied the dynamics of alfalfa growth and its relation with the excessive depletion and resumption of soil water in loess hilly and gully region. The results showed that alfalfa could grow in this region for 10 years, being most flourishing at the forth and fifth year, but declined gradually because of the excessive depletion of soil water. From 0 to 35 cm above ground, the stem biomass was higher than the leaf biomass, and the ratio of stem to leaf was 1.7:1; at 40 cm above ground, the biomass of stem and leaf was equal; and from 45 to 90 cm above ground, the leaf biomass was higher than the stem biomass, with the ratio of leaf to stem 1.42:1. The soil dry layer was not distinct in first two years of alfalfa growth, but getting thicker with time, being from 110 cm in third year to 260 cm in seventh year, with a 4.6%-6.2% of soil water content. It took 5 years for the natural resumption of soil water in degraded alfalfa grassland, and soil water content was increased with time.
本文研究了黄土丘陵沟壑区苜蓿生长动态及其与土壤水分过度消耗和恢复的关系。结果表明,苜蓿在该地区可生长10年,在第4年和第5年最为繁茂,但由于土壤水分过度消耗而逐渐衰退。在地面以上0至35厘米处,茎生物量高于叶生物量,茎与叶的比例为1.7:1;在地面以上40厘米处,茎和叶的生物量相等;在地面以上45至90厘米处,叶生物量高于茎生物量,叶与茎的比例为1.42:1。苜蓿生长的前两年土壤干层不明显,但随着时间的推移逐渐变厚,从第3年的110厘米到第7年的260厘米,土壤含水量为4.6%-6.2%。退化苜蓿草地土壤水分自然恢复需要5年时间,且土壤含水量随时间增加。