PDF Download

[1]LONG Hui-ying,ZHENG Yi-xing,ZHANG Yan-ping,et al.Effect of Different Cover after Irrigation on Soil Moisture and Growth Period of Moringa Oleifera Lam in the Dry-hot Valley of Yunmou, Yunnan Province[J].Research of Soil and Water Conservation,2011,18(01):232-235.

Copy

Effect of Different Cover after Irrigation on Soil Moisture and Growth Period of Moringa Oleifera Lam in the Dry-hot Valley of Yunmou, Yunnan Province

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 18 Number of periods: 2011 01 Page number: 232-235 Column: Public date: 2011-02-20

Title:: Effect of Different Cover after Irrigation on Soil Moisture and Growth Period of Moringa Oleifera Lam in the Dry-hot Valley of Yunmou, Yunnan Province

Author(s):: LONG Hui-ying¹, ZHENG Yi-xing², ZHANG Yan-ping², JIN Jie¹, SHI Liang-tao¹, ZHANG Ming-zhong¹, ZHANG De¹; 1. Institute of Tropical Eco-agricultural Sciences, Yunnan Academy of Agriculture Sciences, Yuanmou, Yunnan 651300, China;
2. Chinese Academy of Forestry Research Institute of Resource Insects, Kunming 650224, China

Keywords:: dry-hot valley; dry slopes field; floor coverings; soil moisture

CLC:: S715.5

DOI:: -

Abstract:: The effect of different cover after irrigation on soil moisture and growth period of Moringa oleifera was studied. The results showed that soil moisture content in 0-20 cm and 20-40 cm depth in mulched plots were higher than those in non-mulched plots for sandy loam and clayey soil, which leading to a decrease of growing stage of Moringa oleifera. Soil moisture content after 10 days’ irrigation in 0-20 cm depth increased 1.2%～4.6% compared to the control for 2-year old Moringa oleifera under plastic films mulch while the value increased 2.6%～3.4% under grass mulch, and soil moisture content increased 1.8%～4.7% for 8-month old Moringa oleifera under plastic films mulch while the value increased 1.8%～4.6% under grass mulch. Additionally, the whole trend of soil moisture content in every soil type was increased with the increase of soil depth. Among three different types of soils of this study, clayey soil had obvious effect on the water-holding capacity.

References:: [1] 欧晓昆.云南省干热河谷区生态环境建设[J].长江流域资源与环境, 1994, 3(3):271-275.
[2] 张建平, 张信宝, 杨忠, 等.云南元谋干热河谷生态环境退化及恢复重建试验研究[J].西南师范大学学报:自然科学版, 2001, 26(6):733-738.
[3] 张映翠.金沙江干热河谷土地资源及其开发潜力[J].山地研究, 1996, 14(3):188-193.
[4] 龙会英, 沙毓沧.干热河谷草和灌木资源引种及综合利用研究[M].昆明:云南科技出版社, 2010(2):203-210.
[5] 张明忠, 朱红业, 张映翠, 等.云南干热河谷旱坡地两种覆盖措施对土壤水分的影响[J].干旱地区农业研究, 2007, 27(3):38-40.
[6] 李保国, 龚元石, 左强, 等.农田土壤水的动态模型及应用[M].北京:科学出版社, 2000:168-180.
[7] 柴宗新, 范建容.金沙江干热河谷植被恢复的思考[J].山地研究, 2001(8):381-384.
[8] 龙会英, 张德, 沙毓沧, 金杰.云南金沙江干热河谷区牧草种质资源的研究利用与开发[J].西南农业学报, 2004, 17(S):313-316.

Similar References:

Memo

Last Update: 1900-01-01