Please use the following format when citing the article: Bogužas V., Sinkevičienė A., Romaneckas K., Steponavičienė V., Skinulienė L., Butkevičienė L. M. 2018. The impact of tillage intensity and meteorological conditions on soil temperature, moisture content and CO 2 efflux in maize and spring barley cultivation. Zemdirbyste-Agriculture, 105 (4): 307-314.
AbstractWith a worldwide increase in the use of sustainable tillage systems, it is important to ascertain their long-term effects on soil properties and greenhouse gas emissions. However, there are not many long-term experiments of this type, and they are conducted in very different climatic and soil conditions. To fill a knowledge gap in this field of study, a long-term, stationary field experiment was set up at Aleksandras Stulginskis University's Experimental Station (54°52ʹ57 N lat., 23°50ʹ51 E long.) in 1988. The current paper presents the experimental data from the 2015-2016 period. The soil of the experimental site is Epieutric Endocalcaric Endogleyic Planosol (PL.gln-can-eup) with a texture of loam on heavy loam. The topsoil layer's characteristics are as follows: pH KCL 6.6-7.0, available phosphorus (P 2 O 5 ) content 131.1-206.7 mg kg -1 , available potassium (K 2 O) content 72.0-126.9 mg kg -1 , humus content 1.68%. This study set out to investigate the effects of long-term application of different tillage systems and meteorological conditions on soil temperature, moisture content and soil surface carbon dioxide (CO 2 ) efflux in the stands of maize and spring barley. The experiment included the following primary tillage methods differing in intensity: 1) conventional ploughing (CP) at a 23-25 cm depth (control treatment), 2) shallow ploughing (SP) at a depth of 12-15 cm, 3) deep cultivation (DC) at a depth of 23-25 cm, 4) shallow cultivation (SC) at a depth of 12-15 cm and 5) no tillage (NT) (direct drilling). The findings of the study suggest that the soil surface CO 2 efflux depended on the amount of rainfall during the crop growing season. In a dry year 2016, the soil CO 2 efflux was lower than that in a wet year, the differences between the tillage treatments were more distinct, with the least flux being from the NT treatment. No significant differences among the tillage treatments were determined in a wet year 2015. The soil temperature depended on the tillage intensity and the weather conditions during the crop growing season. A lower soil temperature was recorded in the reduced tillage treatments compared with conventional tillage treatments. A negative strong correlation was established between the soil surface CO 2 efflux and soil temperature (y = 13.93867 + 0.303x; r = −0.96, P < 0.05). The tillage methods of different intensity did not have significant effect on the moisture content in the soil surface layer; however, in a dry year, the highest moisture content was determined in the no-tillage treatment, while in a wet year the differences were negligible.