Jabro J D, Sainju U, Stevens W B, Evans R G
Northern Plains Agricultural Research Laboratory, USDA-ARS, 1500 N. Central Avenue Sidney, MT 59270, USA.
J Environ Manage. 2008 Sep;88(4):1478-84. doi: 10.1016/j.jenvman.2007.07.012. Epub 2007 Aug 22.
Among greenhouse gases, carbon dioxide (CO(2)) is one of the most significant contributors to regional and global warming as well as climatic change. A field study was conducted to (i) determine the effect of soil characteristics resulting from changes in soil management practices on CO(2) flux from the soil surface to the atmosphere in transitional land from perennial forages to annual crops, and (ii) develop empirical relationships that predict CO(2) flux from soil temperature and soil water content. The CO(2) flux, soil temperature (T(s)), volumetric soil water content (theta(v)) were measured every 1-2 weeks in no-till (NT) and conventional till (CT) malt barley and undisturbed soil grass-alfalfa (UGA) systems in a Lihen sandy loam soil (sandy, mixed, frigid Entic Haplustoll) under irrigated and non-irrigated conditions in western North Dakota. Soil air-filled porosity (epsilon) was calculated from total soil porosity and theta(v) measurements. Significant differences in CO(2) fluxes between land management practices (irrigation and tillage) were observed on some measurement dates. Higher CO(2) fluxes were detected in CT plots than in NT and UGA treatments immediately after rainfall or irrigation. Soil CO(2) fluxes increased with increasing soil moisture (R(2)=0.15, P<0.01) while an exponential relationship was found between CO(2) emission and T(s) (R(2)=0.59). Using a stepwise regression analysis procedure, a significant multiple regression equation was developed between CO(2) flux and theta(v), T(s) (CO(2) flux = e(-3.477+0.123T(s)+6.381theta)(v); R(2)=0.68, P <or= 0.01). Not surprisingly, soil temperature was a driving factor in the equation, which accounted for approximately 59% in variation of CO(2) flux. It was concluded that less intensive tillage, such as no-till or strip tillage, along with careful irrigation management will reduce soil CO(2) evolution from land being converted from perennial forages to annual crops.
在温室气体中,二氧化碳(CO₂)是导致区域和全球变暖以及气候变化的最重要因素之一。开展了一项田间研究,目的是:(i)确定多年生牧草向一年生作物过渡的土地上,土壤管理措施变化所导致的土壤特性对土壤表面向大气排放CO₂通量的影响;(ii)建立根据土壤温度和土壤含水量预测CO₂通量的经验关系。在北达科他州西部灌溉和非灌溉条件下的利亨砂壤土(砂质、混合型、冷性潮湿新成土)中,对免耕(NT)和传统耕作(CT)的麦芽大麦以及未扰动土壤的禾本科-苜蓿(UGA)系统,每1 - 2周测量一次CO₂通量、土壤温度(Tₛ)、土壤容积含水量(θᵥ)。根据总土壤孔隙度和θᵥ测量值计算土壤通气孔隙度(ε)。在某些测量日期,观察到土地管理措施(灌溉和耕作)之间CO₂通量存在显著差异。降雨或灌溉后,CT地块中的CO₂通量立即高于NT和UGA处理。土壤CO₂通量随土壤湿度增加而增加(R² = 0.15,P < 0.01),而CO₂排放与Tₛ之间存在指数关系(R² = 0.59)。使用逐步回归分析程序,建立了CO₂通量与θᵥ、Tₛ之间的显著多元回归方程(CO₂通量 = e⁽⁻³.⁴⁷⁷ ⁺ ⁰.¹²³Tₛ ⁺ ⁶.³⁸¹θ⁾ᵥ;R² = 0.68,P ≤ 0.01)。不出所料,土壤温度是该方程中的驱动因素,约占CO₂通量变化的59%。得出的结论是,减少耕作强度,如免耕或带状耕作,同时进行精细的灌溉管理,将减少从多年生牧草转变为一年生作物的土地上土壤CO₂的排放。