The effects of stubble burning and tillage on soil carbon sequestration and crop productivity in southeastern Australia     

K.Y. Chan  D.P. Heenan 《Soil Use and Management》2005,21(4):427-431

Abstract. In Australia, stubble burning and tillage are two of the major processes responsible for the decline of soil organic carbon concentration in cropped soils, and the resulting soil degradation. However, the relative importance of these two practices in influencing the soil organic carbon concentration and the long-term impact on soil quality and productivity are not clear. The effects of stubble burning as practised by farmers in southeastern Australia were evaluated in two field trials, one of 19 years duration, the other of 5 years. Conventional tillage (three tillage passes) led to greater loss of soil organic carbon than stubble burning. Loss of total soil organic carbon attributed to stubble burning in the 0–10 cm layer was estimated to be 1.75 t C ha⁻¹ over the period of the 19-year trial, equivalent to 29% of that lost due to tillage. In the 5-year trial, no change in soil organic carbon due to stubble burning was detectable. Changes in soil quality associated with stubble burning detected in the longer trial included a reduction in macro-aggregate stability, and increases in pH and exchangeable K⁺. Only the latter two were detected in the shorter trial. A higher mean wheat yield (average 0.15 t ha⁻¹) following stubble burning was observed in the 19-year trial but not in the 5-year trial. Research to monitor the longer term effects of stubble burning is needed, and to identify conditions where loss of soil organic carbon is minimized.  相似文献   

Issues and Some Strategies of Sustainable Development of Black Soil Resources in Black Soil Zone in Northeast China     

贾利 《勤云标准版测试》2005,(4)

黑土资源是世界的稀缺资源,黑土带的水土流失、环境污染、土地流转、土地退化问题成为黑土资源可持续发展的障碍。根据实地调研结合资料,分析了东北黑土带土地资源可持续发展的主要问题;提出了黑土资源的可持续发展对策,即:加强农业发展规划;保护黑土区耕地,农耕技术上改进,加强农田基本建设等。  相似文献   

Quantitative site classification in the key county in the conversion of farmland to forests project     

Shidong Li  Guofang Shen  Mingpu Zhai  Junqing Li 《Frontiers of Forestry in China》2006,1(2):157-162

According to the requirements of the conversion of farmland to forests project (CFFP), we investigated the vegetation factors and environmental factors from more than 6,105 sub-compartments in Liangcheng County, Inner Mongolia by using the Matlab, analytic hierarchy process (AHP), and the hierarchical cluster method (HCM). The site conditions were classified quantitatively. The results show that CFFP at this site comprises five site-type groups and 19 site types. A quantitative site classification system method has been established in this paper. __________ Translated from Journal of Beijing Forestry University, 2005, 27(6) [译自: 北京林业大学学报, 2005, 27(6)]  相似文献   

福建土壤对酸沉降的相对敏感性评价与区划     

樊后保 《福建林学院学报》2001,21(3):198-202

选择母岩、土壤类型、土地利用和降雨量 4个生态因子 ,应用半定量化方法对其进行类目划分和权重 ,综合评价了福建省土壤对酸沉降的相对敏感性 ,并应用地理信息系统进行了区划 .由于福建省风化缓慢的硅质岩所占的比例较大 ,土壤大多呈酸性至微酸性反应 ,降水丰富 ,加之针叶林面积大 ,所以全省有 60 %以上面积的土壤显示出较大的敏感性等级 (5～ 7级 )  相似文献   

Residue management for reducing evaporation in relation to soil type and evaporativity1     

S.S. Prihar  S.K. Jalota  J.L. Steiner 《Soil Use and Management》1996,12(3):150-157

Abstract. Usual residue-management options are to remove the residue, use it as mulch with or without undercutting or to incorporate it into the soil. While the role of surface mulch in evaporation has been widely studied, the information on the effect on evaporation of mulch with undercutting or residue incorporated into soil, particularly in relation to soil type and evaporativity (E_o) is lacking. We studied the effect of wheat straw used in various ways on the course of evaporation loss from soil columns with three soils at Ludhiana, India and one soil at Bushland, Texas, USA, under two E_o's Energy-limited evaporation rates under mulch (E_om) followed the soil-specific relation E_om/E_o= a e^(bRes+cEo), where Res is residue rate t/ha and a, b and c are constants; E_o, is expressed in mm/d. In an effort to model the total evaporation (CE) during the energy-limited stage ‘U’ was obtained from appropriate CE versus time curves and (CE-U) was regressed over (t - ti)^0.5 to obtain the slope ‘α’ (Ritchie 1972) for the soil-limited evaporation stage. The observed ‘U’ was independent of mulch rate and E_o but was strongly affected by soil type, Values of ‘α’ decreased with increase in mulch rate and decrease in E_o and coarseness of soil. The otherwise short lived benefit of evaporation reduction with mulch per se, which peaked after a few days was maintained when residue was mixed with soil at the stage when evaporation reduction reached a maximum; this benefit continued for several weeks. Cumulative evaporation values computed from ‘U’ and ‘α’ agreed closely with the observed values under straw mulch for loamy sand and clay loam soils and for ‘undercut’ and ‘residue mixed’ treatments on all soils regardless of E_o, and for all situations under small E_o. However, for sandy loam and silt loam soils under E_o of 10 mm/d, the modified square root of the time function of Jalota et al. (1988) gave a better fit.  相似文献   

重迎茬亚麻生长发育障碍机制的研究   总被引：2，自引：0，他引：2  

杨学 《黑龙江农业科学》2004,(3):24-26

重迎茬亚麻减产是由多种因素综合作用的结果,亚麻重迎茬可使病害加重是最主要因素,重茬年限越久发病越严重;重迎茬造成了土壤营养元素的单一消耗,随着重迎茬年限的增加,土壤中速效氮、速效磷、速效钾等含量降低。  相似文献   

河西走廊盐渍化草地土壤生态指标的选择与分类     

闫顺国 《草业科学》1991,8(3):22-25

  相似文献   

农用地因素法与样地法分等对比研究——以重庆市丰都县为例     

刘燕红陈务魁  胡渝清王玥 《四川畜牧兽医学院学报》2006,4(1):8-11

对现行《农用地分等规程》中因素法和样地法进行探讨，寻求农用地分等的最佳方法。文献资料法、比较分析法。《规程》中因素法分等使得研究区单元分值出现拐点，划分等别部分与实际不符；样地法分等结果则不存在这一问题。在农用地分等中，在县域内种植制度为一年两熟和一年一熟的地区采用样地法分等更合理。  相似文献   

实验猴志贺氏菌检出、血清分型及药物敏感性试验   总被引：1，自引：0，他引：1  

盘宝进  汪文龙  谢永平  韦梅良  罗兆飞  陈立标 《广西农业科学》2006,37(3):331-332

采用实验动物国家标准(GB/T 14926.47-2001)的检验方法,对144份待出口实验猴粪便样品检测,检出志贺氏菌2株,阳性检出率1.39%。血清学分型,均属于B群志贺氏菌,血清型分别为X变种和Y变种。药敏试验结果表明,2株分离菌对先锋V、氟哌酸和环丙沙星高度敏感,而对青霉素、红霉素和复方新诺明耐药。  相似文献   

覆盖免耕在休闲期的节水和生育期的调温效应   总被引：10，自引：2，他引：8  

姚宝林  景明  施炯林 《甘肃农业大学学报》2005,40(2):208-211

对免耕覆盖、秸秆还田和常规耕作在休闲期的节水效果研究表明:在夏季休闲期,免耕覆盖比常规耕作多贮水30.62mm,比秸秆还田多23.91mm;在冬季储水灌溉期间,可将储水定额从2100m3/hm2减少到600和975m3/hm2。对春小麦生育期土壤表层,5、10、15、20和25cm处温度变化观测发现:免耕覆盖土壤温度在气温较低的8:00可以提高土壤表层温度,在气温较高的14:00可以减缓土壤温度的升高,而在19:00气温降低时可以减缓土壤温度的降低,使土壤温度一直保持在一个稳定的状态,这有利于调节农田小气候,创造作物良好的生长环境。  相似文献