DEPTH DISTRIBUTION OF SOIL ORGANIC CARBON FRACTIONS IN RELATION TO TILLAGE AND CROPPING SEQUENCES IN SOME DRY LANDS OF PUNJAB, PAKISTAN

被引:32
作者
Hassan, Asma [1 ,2 ]
Ijaz, Shahzada Sohail [1 ,2 ]
Lal, Rattan [3 ]
Ali, Safdar [1 ,2 ]
Hussain, Qaiser [1 ,2 ]
Ansar, Muhammad [1 ,2 ]
Khattak, Romaan Hayat [4 ]
Baloch, Muhammad Sharif [1 ,2 ]
机构
[1] PMAS Arid Agr Univ, Dept Soil Sci, Rawalpindi, Pakistan
[2] PMAS Arid Agr Univ, SWC, Rawalpindi, Pakistan
[3] Ohio State Univ, Carbon Management & Sequestrat Ctr C MASC, Columbus, OH 43210 USA
[4] Quaid I Azam Univ, Dept Anim Sci, Islamabad, Pakistan
关键词
depth distribution; soil organic carbon fractions; conservation agriculture; potentially mineralizable C; particulate organic C; HCl insoluble C; Punjab; LONG-TERM TILLAGE; MICROBIAL BIOMASS; CONSERVATION TILLAGE; N MINERALIZATION; MATTER; ROTATION; SEQUESTRATION; RESIDUE; RESPIRATION; STABILITY;
D O I
10.1002/ldr.2345
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Depth distribution of soil organic carbon (SOC) fractions depends on the efficiency of agro-technical managements. Information on depth distribution of SOC fractions mostly confined to the plow layer and scant in dry lands of Punjab, Pakistan. Therefore, a field experiment was laid out with moldboard plow (MP) (control), tine cultivator (TC), and minimum tillage (MT) as main plots, and cropping sequences fallow wheat (Triticum aestivum L.), (FW, control), mungbean (Vigna radiata L.) wheat (MW), sorghum (Sorghum bicolor L.) wheat (SW), green manure wheat (GW), and mungbean-chickpea (MC) (Cicer arietinum L.) as sub-plots. Treatment effects were assessed for microbial biomass carbon (MBC), potentially mineralizeable carbon (PMC), particulate organic carbon (POC), dissolved organic carbon (DOC), HCl insoluble carbon (HIC), and stratification ratio (SR) in Rawal series: Udic Haplustalf. Alfisols. The MBC concentration was the highest in MT system, at 15 to 30-cm depth under MW and PMC concentration was highest under SW with MT at 45-60 cm. MP had higher POC in FW sequence. The highest DOC was at 0 to 15-cm depth under MC with TC and stock of HIC was more under TC with FW sequence. The highest SR of PMC was under MT with FW at 0-15: 15-30 and POC was under TC and MP with FW at depths of 0-15: 45-60 cm. The highest SR for DOC was under MP with GW at 0-15: 45-60 cm and HCl insoluble C was under MT with SW at 0-15: 45-60. In broad-spectrum, labile organic fractions revealed differential sensitivity, and POC stocks are also a sensitive indicator to detect the short-management effects. Copyright (C) 2015 John Wiley & Sons, Ltd.
引用
收藏
页码:1175 / 1185
页数:11
相关论文
共 62 条
[1]   Tillage and cropping effects on soil organic carbon in Mediterranean semiarid agroecosystems: Testing the Century model [J].
Alvaro-Fuentes, J. ;
Lopez, M. V. ;
Arrue, J. L. ;
Moret, D. ;
Paustian, K. .
AGRICULTURE ECOSYSTEMS & ENVIRONMENT, 2009, 134 (3-4) :211-217
[2]  
Anderson J.M., 1993, TROPICAL SOIL BIOL F
[3]  
[Anonymous], SOIL SER KEY SOIL CL
[4]   NATURAL C-13 ABUNDANCE AS A TRACER FOR STUDIES OF SOIL ORGANIC-MATTER DYNAMICS [J].
BALESDENT, J ;
MARIOTTI, A ;
GUILLET, B .
SOIL BIOLOGY & BIOCHEMISTRY, 1987, 19 (01) :25-30
[5]   Long-term tillage and crop rotation effects on microbial biomass and C and N mineralization in a Brazilian Oxisol [J].
Balota, EL ;
Colozzi, A ;
Andrade, DS ;
Dick, RP .
SOIL & TILLAGE RESEARCH, 2004, 77 (02) :137-145
[6]   Long-term cropping systems and tillage management effects on soil organic carbon stock and steady state level of C sequestration rates in a semiarid environment [J].
Barbera, V. ;
Poma, I. ;
Gristina, L. ;
Novara, A. ;
Egli, M. .
LAND DEGRADATION & DEVELOPMENT, 2012, 23 (01) :82-91
[7]   PROJECTED CHANGES IN SOIL ORGANIC CARBON STOCKS UPON ADOPTION OF RECOMMENDED SOIL AND WATER CONSERVATION PRACTICES IN THE UPPER TANA RIVER CATCHMENT, KENYA [J].
Batjes, N. H. .
LAND DEGRADATION & DEVELOPMENT, 2014, 25 (03) :278-287
[8]   Particulate organic matter, carbohydrate, humic acid contents in soil macro- and microaggregates as affected by cultivation [J].
Bongiovanni, Marcos D. ;
Lobartini, Juan C. .
GEODERMA, 2006, 136 (3-4) :660-665
[9]  
Brady N.C., 2008, The nature and properties of soils, P518
[10]  
Camberdella CA, 1992, SOIL SCI SOC AM J, V76, P395