WU Xianzhong1, 2, LI Yi1. Effects of Film Mulching on Soil Moisture and Temperature Changes during Plant Dormancy Period in Semiarid Loess Hilly Region[J]. 2017, 31(3): 182-186.
DOI:
WU Xianzhong1, 2, LI Yi1. Effects of Film Mulching on Soil Moisture and Temperature Changes during Plant Dormancy Period in Semiarid Loess Hilly Region[J]. 2017, 31(3): 182-186. DOI: 10.13870/j.cnki.stbcxb.2017.03.031.
Effects of Film Mulching on Soil Moisture and Temperature Changes during Plant Dormancy Period in Semiarid Loess Hilly Region
A field test was conducted at the Mizhi Experimental Station of Northwest A & F University from October 2014 to April 2015
to research the soil moisture movement law and temperature difference under different plastic film mulching in plant dormancy period in semiarid loess hilly region. No plastic film mulching (CK) and transparent film mulching (TF) treatments were set up at the same level of terraces at the depth of 0-400 cm to observe soil moisture movement. Three treatments
including CK
TF
and black film covering (BF) were designed at the same level at the depth of 0-50 cm (15 cm
30 cm
50 cm) to observe soil temperature. The results showed that soil water storage capacity of TF was 51.9% higher than that of CK at the depth of 0-400 cm in the dormancy period
and the difference was significant (p < 0.05). The maximum amplitude of soil water storage appeared at the depth of 0-20 cm
and soil water storage at the depth of 20-60 cm decreased from 54.9% to 26.3%. In typical sunny days
the maximum temperature difference between the three treatments of CK
TF
and BF was 2.25-2.7 oC
3.45-3.5 oC
and 1.5-1.8 oC at the non-freezing stage. Whereas the difference was 1.65 oC
2.1 oC and 1.2 oC at the freezing stage
and the effect of film insulation was not obvious when the soil was frozen. The depth of film insulation was up to 15 cm
the warming effect of BF treatment was better than that of TF. The above evidences suggested that the plastic film mulching in plant dormancy period could increase soil moisture and soil temperature
reduce soil water loss and promote water deep infiltration in the 0-20 cm soil layer. Furthermore
BF treatment might be more favorable for warming and stabilizing temperature change than TF treatment.
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WU Yong-long1,WANG Xin-ai2,LI Yong-sheng2,DU Jian-jun2,LI Feng3,NIE Ji-yun1(1.Institute of Pomology,Chinese Academy of Agricultural Sciences,Xingcheng,Liaoning 125100,2.Research Center for Plant Nutrition and New Fertilizer,Zhongkai University of Agricultural and Engineering,Guangzhou,Guangdong 510225,3.Research Center of Shenzhen Batian Ecotypic Engineering Co.,Ltd.,,)
CHEN Jian-qiu1,2,CHEN Hong-kun2,ZHANG Min1,SUN De-fang2,CHEN Hai-ning1,WANG Li-ping2(1.College of Resources and Environment,Shandong Agricultural University,Chinese NationalEngineering Research Center for Slow/Controlled Release Fertilizer,State Key Laboratory of Crop Biology,Taian,Shandong 271018,2.Shandong Kingenta Ecological Engineering Co.,Ltd.,,)