1. 山西农业大学资源与环境学院, 山西 太谷,030801
2. 山西农业大学农业资源与环境国家级实验教学示范中心, 山西 太谷,030801
[ "何冰(1993-),女,河北邢台人,硕士研究生,主要从事土壤肥力与环境研究。E-mail:15200031194@163.com" ]
纸质出版:2018
移动端阅览
何冰, 李廷亮, 栗丽, 等. 采煤塌陷区复垦土壤团聚体碳氮分布对施肥的响应[J]. 水土保持学报, 2018,32(4):184-189.
HE Bing, LI Tingliang, LI Li, et al. Response of Carbon and Nitrogen Distribution of Reclaimed Soil Aggregates to Fertilizers in Coal Mining Subsidence Area[J]. 2018, 32(4): 184-189.
何冰, 李廷亮, 栗丽, 等. 采煤塌陷区复垦土壤团聚体碳氮分布对施肥的响应[J]. 水土保持学报, 2018,32(4):184-189. DOI: 10.13870/j.cnki.stbcxb.2018.04.029.
HE Bing, LI Tingliang, LI Li, et al. Response of Carbon and Nitrogen Distribution of Reclaimed Soil Aggregates to Fertilizers in Coal Mining Subsidence Area[J]. 2018, 32(4): 184-189. DOI: 10.13870/j.cnki.stbcxb.2018.04.029.
为了揭示长期不同培肥措施下采煤塌陷区复垦土壤团聚体有机碳氮含量的变化规律,通过干筛法研究了不施肥(CK)、单施有机肥(M)、单施化肥(CF)、有机肥与化肥配施(MCF)、生物有机肥与化肥配施(MCFB)5种培肥措施下复垦4年和8年土壤各粒级团聚体分布组成特征以及各团聚体有机碳氮含量的变化规律。结果表明,复垦土壤团聚体含量随粒级减小呈先减小后增大的变化趋势,其中以3~2 mm粒级团聚体含量最低,占团聚体总量2%~3%,以2~1 mm粒级团聚体含量最高,占团聚体总量25%~31%。不同培肥措施下复垦4年和8年土壤团聚体分布特征无明显差异,但较未复垦生土明显降低了>7 mm和7~5 mm团聚体含量。复垦8年土壤的平均重量直径(MWD)、几何平均直径(GMD)高于复垦4年土壤,分形维数(D)值低于复垦4年土壤。各培肥处理间以单施有机肥MWD、GMD值最高,D值最低。各培肥处理土壤团聚体有机碳氮含量随粒径减小递增,以0.5~0.25 mm粒径团聚体最高,而有机碳储量以2~1 mm粒级团聚体最高,分别占24.2%~33.8%和17.0%~33.1%。各处理间有机碳氮含量以单施有机肥处理最高,但不同处理间有机碳氮储量无显著差异。总体表明,采煤塌陷区复垦4年和8年土壤团聚体分布特征及碳氮储量无明显变化,单施有机肥可提高复垦土壤团聚体有机碳氮含量及团聚体稳定性。
In order to reveal the changes of organic carbon and nitrogen content of reclaimed soil aggregates in coal mining subsidence areas under long-term fertilization measures
we examined the characteristics of soil aggregates distribution and the changes of organic carbon and nitrogen contents in 4 years and 8 years of reclamation soil under five fertilization measures
which were non-fertilizer (CK)
single application of manure fertilizer (M)
single application of chemical fertilizer (CF)
manure fertilizer and chemical fertilizer (MCF)
biological organic fertilizer and chemical fertilizer mixed fertilizer (MCFB). The results showed that the content of reclaimed soil aggregates first decreased and then increased with the decreasing of grain size
in which the content of aggregates with the size of 3~2 mm was the lowest
accounting for 2%~3% of the total aggregates
and the content of aggregates with the size of 2~1 mm was the highest
accounting for 25%~31%. There was no significant difference in the distribution characteristics of soil aggregates between the 4 years and 8 years of reclaimation under different fertilization measures
but the contents of 7~5 mm and >7 mm aggregates significantly decreased compared with unreclaimed raw soil. The mean weight diameter (MWD) and geometric mean diameter (GMD) of the 8 years reclaimation soil were both higher than those of 4 years
while the fractal dimension (D) value was lower than that of 4 years. The MWD and GMD values of M treatment were the highest
but the D of it was the lowest. The contents of organic carbon and nitrogen in soil aggregates increased with the decreasing of soil aggregate size in reclaimed soil. The aggregates with the size of 0.5~0.25 mm were the highest
while the organic carbon and nitrogen storages in the aggregates with the size of 2~1 mm were the highest
accounting for 24.2%~33.8% and 17.0%~33.1%
respectively. Organic carbon and nitrogen contents were the highest in M treatment
but there was no significant difference in the storages of organic carbon and nitrogen between different treatments. Thus
there was no significant change in the distribution characteristics of soil aggregates and carbon and nitrogen reserves in the 4 years and 8 years reclaimed lands of coal mining subsidence area. The application of manure fertilizer could increase the organic carbon and nitrogen content and the stability of the reclaimed soil aggregates.
李文军,杨基峰,彭保发,等.施肥对洞庭湖平原水稻土团聚体特征及其有机碳分布的影响[J].中国农业科学,2014,47(20):4007-4015.
何淑勤,郑子成.不同土地利用方式下土壤团聚体的分布及其有机碳含量的变化[J].水土保持通报,2010,30(1):7-10.
韩志卿,韩志才,张电学,等.不同施肥制度下褐土微团聚体碳氮分布变化及其对肥力的影响[J].华北农学报,2008,23(4):190-195.
Kundu N K,Ghose M K. Soil profile characteristic in Rajmahal Coalfield area[J]. Indian Journal of Soil and Water Conservation,1997,25:28-32.
李君剑,严俊霞,李洪建.矿区不同复垦措施对土壤碳矿化和酶活性的影响[J].生态学报,2015,35(12):4178-4185.
刘京,常庆瑞,李岗,等.连续不同施肥对土壤团聚体性影响的研究[J].水土保持通报,2000,20(4):24-26.
王仁杰,强久次仁,薛彦飞,等.长期有机无机肥配施改变了嵝土团聚体及其有机和无机碳分布[J].中国农业科学,2015,48(23):4678-4689.
谭秋锦,宋同清,彭晚霞,等.峡谷型喀斯特不同生态系统土壤团聚体稳定性及有机碳特征[J].应用生态学报,2014,25(3):671-678.
孙天聪,李世清,邵明安.长期施肥对褐土有机碳和氮素在团聚体中分布的影响[J].中国农业科学,2005,38(9):1841-1848.
赵红,袁培民,吕贻忠,等.施用有机肥对土壤团聚体稳定性的影响[J].土壤,2011,43(2):306-311.
Nimmo J R,Perkins K S.Aggregate stability and size distrib-ution[J].Methods of Soil Analysis:Part4,Physical Methods,2002,4:317-328.
周虎,吕贻忠,杨志臣,等.保护性耕作对华北平原土壤团聚体特征的影响[J].中国农业科学,2007,40(9):1973-1979.
姜灿烂,何园球,刘晓利,等.长期施用有机肥对旱地红壤团聚体结构与稳定性的影响[J].土壤学报,2010,47(4):716-722.
易亚男,尹力初,张蕾,等.施肥对不同地下水位水稻土团聚体组成及有机碳分布的影响[J].水土保持学报,2013,27(5):144-153.
鲍士旦.土壤农化分析[M].北京:中国农业出版社,2000.
李辉信,袁颖红,黄欠如,等.不同施肥处理对红壤水稻土团聚体有机碳分布的影响[J].土壤学报,2006,43(3):422-427.
冷延慧,汪景宽,李双异.长期施肥对黑土团聚体分布和碳储量变化的影响[J].生态学杂志,2008,27(12):2171-2177.
邢旭明,王红梅,安婷婷,等.长期施肥对棕壤团聚体组成及其主要养分赋存的影响[J].水土保持学报,2015,29(2):267-273.
吕欣欣,丁雪丽,张彬,等.长期定位施肥和地膜覆盖对棕壤团聚体稳定性及其有机碳含量的影响[J].农业资源与环境学报,2018,35(1):1-10.
李辉信,袁颖红,黄欠如,等.不同施肥处理对红壤水稻土团聚体有机碳分布的影响[J].土壤学报,2006,43(3):422-429.
刘敏英.植茶年限对土壤团聚体组成及其有机碳组分影响.成都:四川农业大学,2012.
刘中良,宇万太,周桦,等.长期施肥对土壤团聚体分布和养分含量的影响[J].土壤,2011,43(5):720-728.
高会议,郭胜利,刘文兆,等.不同施肥处理对黑垆土各粒级团聚体中有机碳含量分布的影响[J].土壤学报,2010,47(5):931-938.
陈晓芬,李忠佩,刘明,等.不同施肥处理对红壤水稻土团聚体有机碳、氮分布和微生物生物量的影响[J].中国农业科学,2013,46(5):950-960.
樊红柱,秦鱼生,陈庆瑞,等.长期施肥紫色水稻土团聚体稳定性及其固碳特征[J].植物营养与肥料学报,2015,21(6):1473-1480.
0
浏览量
1066
下载量
13
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621