|Table of Contents|

Analysis of Temporal-spatial Variation and Climate Influencing Factors on Wine Grape Water Requirement in Gansu Province During the Past 30 Years(PDF)

《北方园艺》[ISSN:1001-0009/CN:23-1247/S]

Issue:
2015年10
Page:
190-195
Research Field:
Publishing date:

Info

Title:
Analysis of Temporal-spatial Variation and Climate Influencing Factors on Wine Grape Water Requirement in Gansu Province During the Past 30 Years
Author(s):
LI Ya-shanWANG Zhen-jiFAN Shu-guoWANG BoXU Cheng-dong
(Department of Chemistry and Life Science,Chuxiong Normal University,Chuxiong,Yunnan 675000)
Keywords:
Gansu provincewine grapecrop water requirementcrop coefficientmeteorological factors
PACS:
S 274.3;S 663.1
DOI:
10.11937/bfyy.201510048
Abstract:
Crop water requirement was the precondition of irrigation decision-making.To research the temporal-spatial variations of crop water requirement and the influencing factors of crop water requirement had an important guiding function on the irrigation water management.Crop water requirement of wine grape in Gansu province were calculated by FAO approach,which equaled to reference crop evapotranspiration multiplied by crop coefficient of wine grape.Meantime,the relation between crop water requirement and meteorological factors were explored.The results suggested that the spatial distribution of water requirement of wine grape in Gansu province emerged higher in northwest and lower in southeast.The water requirement of wine grape was concentrated upon the range of 300-600 mm.The highest space was twice than the lowest space.From nearly 30 years,the water requirement of wine grape in Gansu province presented rising trend,and the rising rate was 5.64 mm/10a,but the trend was not significant.But the local areas of the province appeared rising or decreasing significantly.Correlation analysis relative showed that daily average temperature,daily maximum temperature,daily minimum temperature sunshine hour and wind speed were significantly positive correlated with wine grape water requirement,while relative humidity and precipitation were significantly negatively correlated with it.The daily average temperature was most correlative with wine grape water requirement and the precipitation was the last correlative with it among the seven meteorological factors.

References:


[1]高晓容,王春乙,张继权,等.近50年东北玉米生育阶段需水量及旱涝时空变化[J].农业工程学报,2012,28(12):101-109.
[2]尹海霞,张勃,王亚敏,等.黑河流域中游地区近43年来农作物需水量的变化趋势分析[J].资源科学,2012,34(3):409-417.
[3]黄晚华,杨晓光,曲辉辉,等.基于作物水分亏缺指数的春玉米季节性干旱时空特征分析[J].农业工程学报,2009,25(8):28-34.
[4]李春强,李保国,洪克勤.河北省近35年农作物需水量变化趋势分析[J].中国生态农业学报,2009,17(2):359-363.
[5]刘宏谊,马鹏里,杨兴国,等.甘肃省主要农作物需水量时空变化特征分析[J].干旱地区农业研究,2005,23(1):39-44.
[6]王鹤龄,王润元,张强,等.气候变暖对甘肃省不同气候类型区主要作物需水量的影响[J].中国生态农业学报,2011,19(4):886-871.
[7]Allen R G,Pereira L S,Raes D,et al.Crop evapotranspiration:guidelines for computing crop water requirements[R].FAO Irrigation and Drainage Paper 56,Rome,1998.
[8]Romero P,Martinez-Cutillas A.The effects of partial root-zone irrigation and regulated deficit irrigation on the vegetative and reproductive development of field-grown Monastrell grapevines[J].Irrig Sci,2012,30:377-396.
[9]魏凤英.现代气候统计诊断与预测技术[M].2版.北京:气象出版社,2007:63-65.
[10]顾世祥,李远华,何大明,等.近45年元江干热河谷灌溉需水的变化趋势分析[J].水利学报,2007,38(12):1512-1518.
[11]曹雯,申双和,段春峰.中国西北潜在蒸散时空演变特征及其定量化成因[J].生态学报,2012,32(11):3394-3403.
[12]范晓辉,郝智文,王孟本.山西省近50年日照时数时空变化特征研究[J].生态环境学报,2010,19(3):605-609.
[13]李政,苏永秀.1961—2004年广西降水的变化特征分析[J].中国农学通报,2009,25(15):268-272.
[14]李胜,曹孜义,张金文,等.兰州地区酿酒葡萄品种引种试验初报[J].农业工程学报,2004,20(增刊):126-129.
[15]马兴祥,魏育国,蒋菊芳.沙漠边缘酿造葡萄生长气象条件及生态响应[J].中国生态农业学报,2007,15(5):11-16.
[16]闫博远.干旱荒漠绿洲区根系分区交替灌溉对葡萄生长和品质的影响[D].北京:中国农业大学,2007.
[17]Sen P K.Estimates of the regression coefficient based on Kendall’s tau[J].J Am Stat Assoc,1968,63:1379-1389.
[18]王澄海,李健,许晓光.中国近50年气温变化准3年周期的普遍性及气温未来的可能变化趋势[J].高原气象,2012,31(1):126-136.
[19]汪志红,张霞,王冀.IPCC-AR4模式对中国21世纪气候变化的情景预估[J].地理研究,2008,27(4):787-799.

Memo

Memo:
-
Last Update: 2015-08-09