Responses of soil respiration to changes in depth of seasonal frozen soil in Ebinur Lake area, arid area of Northwest China

2013 ◽  
Vol 33 (22) ◽  
pp. 7259-7269
Author(s):  
秦璐 QIN Lu ◽  
吕光辉 Lü Guanghui ◽  
何学敏 HE Xuemin ◽  
张雪妮 ZHANG Xueni ◽  
张雪梅 ZHANG Xuemei ◽  
...  
2015 ◽  
Vol 48 (8) ◽  
pp. 871-880 ◽  
Author(s):  
L. Qin ◽  
G. H. Lv ◽  
X. M. He ◽  
J. J. Yang ◽  
H. L. Wang ◽  
...  

2018 ◽  
Vol 22 (5) ◽  
pp. 3075-3086 ◽  
Author(s):  
Guanghui Ming ◽  
Hongchang Hu ◽  
Fuqiang Tian ◽  
Zhenyang Peng ◽  
Pengju Yang ◽  
...  

Abstract. Plastic film mulching (PFM) has widely been used around the world to save water and improve crop yield. However, the effect of PFM on soil respiration (Rs) remains unclear and could be further confounded by irrigation and precipitation. To address these topics, controlled experiments were conducted in mulched and non-mulched fields under drip irrigation from 2014 to 2016 in an arid area of the Xinjiang Uygur Autonomous Region, northwest China. The spatio-temporal pattern of soil surface CO2 flux as an index of soil respiration under drip irrigation with PFM was investigated, and the confounded effects of PFM and irrigation/precipitation on soil respiration were explored. The main findings were as follows. (1) Furrows, planting holes, and plastic mulch are three important pathways of soil CO2 emissions in mulched fields, of which the planting hole efflux outweighs that from the furrow, with the largest values of 8.0 and 6.6 µmol m−2 s−1, respectively, and the plastic mulch itself can emit up to 3.6 µmol m−2 s−1 of CO2. (2) The frequent application of water (i.e. through irrigation and precipitation) elevates soil moisture and soil respiration and enhances their variation. The resultant higher variation of soil moisture further alleviates the sensitivity of soil respiration to soil temperature, leading to a weak correlation and lower Q10 values. (3) Soil CO2 effluxes from furrows and ridges in mulched fields outweigh the corresponding values in non-mulched fields in arid areas. However, this outweighing relation attenuates with increasing precipitation. Furthermore, by combining our results with those from the literature, we show that the difference in soil CO2 effluxes between non-mulched and mulched fields presents a linear relation with the amount of precipitation, which results in negative values in arid areas and positive values in humid areas. Therefore, whether PFM increases soil respiration or not depends on the amount of precipitation during the crop-growing season.


2017 ◽  
Author(s):  
Guanghui Ming ◽  
Hongchang Hu ◽  
Fuqiang Tian ◽  
Zhenyang Peng ◽  
Pengju Yang ◽  
...  

Abstract. Plastic film mulching (PFM) has been widely used for saving water and improving yield around the world, particularly in arid areas. However, the effect of PFM in agriculture on soil respiration is still unclear, and this effect may be confounded with irrigation and precipitation. To detect the effects of PFM, irrigation and precipitation on the temporal and spatial variations in soil respiration, plastic mulched and non-mulched drip irrigation contrast experiments were conducted in the arid area of the Xinjiang Uygur Autonomous Region, Northwest China. PFM generated more complicated spatial heterogeneity in the microclimate with increased albedo, improved soil temperature, soil moisture and crop growth, and led to the stronger spatial heterogeneity of the soil respiration. The soil respiration in the plant holes was larger than in the furrows, and plastic mulch itself can emit up to 2.75 μmol m−2 s−1 CO2, which indicates that furrows, plant holes and plastic mulch were the important pathways for CO2 emissions in the mulched field. Frequent irrigation and precipitation made the soil respiration much more dynamic and fluctuated. The sensitivity of the soil respiration to soil temperature was weakened by extreme variations in the soil moisture with lower correlation and Q10 values. In the wetting-drying cycle, both irrigation and precipitation restrained the soil respiration at a high soil water content (SWC) with a threshold of 60 % water-filled pore space (WFP) in the furrows and 50 % WFP in the ridges, and the restrain effect decreased gradually with the depleting of soil moisture. The accumulated soil respiration calculated from the area ratio of the different parts in the furrows and ridges in the mulched field were both larger than in the non-mulched field during the growing season. However, this magnitude decreased with increasing precipitation over three experimental years. It was speculated that the effect of drip irrigation on the soil respiration was primarily on the ridges while the effect of precipitation mostly concentrated in the furrows and ridges in the non-mulched field because of the mulch barrier. Therefore, the precipitation accelerated more respiration in the mulched than in the non-mulched field. The difference in soil respiration between the mulched and non-mulched fields was observed to have a positive correlation with precipitation per the findings of other studies. In a humid climate with much more precipitation, soil respiration in the non-mulched field can also exceed that of the mulched field and explains why certain studies concluded that plastic mulch decreased soil respiration. The above results indicate that both irrigation and precipitation alter soil respiration and this effect can be modified by plastic mulch. Therefore, whether the PFM increases soil respiration compared to a non-mulched field largely depends on precipitation in the field.


2014 ◽  
Vol 11 (2) ◽  
pp. 259-268 ◽  
Author(s):  
B. Wang ◽  
T. S. Zha ◽  
X. Jia ◽  
B. Wu ◽  
Y. Q. Zhang ◽  
...  

Abstract. The current understanding of the responses of soil respiration (Rs) to soil temperature (Ts) and soil moisture is limited for desert ecosystems. Soil CO2 efflux from a desert shrub ecosystem was measured continuously with automated chambers in Ningxia, northwest China, from June to October 2012. The diurnal responses of Rs to Ts were affected by soil moisture. The diel variation in Rs was strongly related to Ts at 10 cm depth under moderate and high volumetric soil water content (VWC), unlike under low VWC. Ts typically lagged Rs by 3–4 h. However, the lag time varied in relation to VWC, showing increased lag times under low VWC. Over the seasonal cycle, daily mean Rs was correlated positively with Ts, if VWC was higher than 0.08 m3 m−3. Under lower VWC, it became decoupled from Ts. The annual temperature sensitivity of Rs (Q10) was 1.5. The short-term sensitivity of Rs to Ts varied significantly over the seasonal cycle, and correlated negatively with Ts and positively with VWC. Our results highlight the biological causes of diel hysteresis between Rs and Ts, and that the response of Rs to soil moisture may result in negative feedback to climate warming in desert ecosystems. Thus, global carbon cycle models should account the interactive effects of Ts and VWC on Rs in desert ecosystems.


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