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Difference in Effects of Different Manure Application on Soil Physical Properties of Sloping Farmland in Black Soil Area
REYIHANGULIKadier, ZHOUYinuo, ZHANGYi, ZHANGZiwei, XINGRuping, MAXin, XUChong, LIUWenli, WUJinggui, LIJianming
PDF(1470 KB)
PDF(1470 KB)
Difference in Effects of Different Manure Application on Soil Physical Properties of Sloping Farmland in Black Soil Area
To investigate the effects of applying different livestock manure on the physical properties of sloping cropland soil in the black soil area, chemical fertilizers were used as the control, and three kinds of livestock manure, namely, chicken manure, hog manure and cow manure, were selected for the field experiment. The results showed that the application of livestock manure reduced soil bulk weight, whereas it increased soil aggregates, capillary porosity, soil water content and soil infiltration in cultivated land on black soil slopes, and there were differences among different livestock manures. Compared with the CK (control) group, the chicken manure group had a significant increase in 1-0.5 mm soil aggregate particle size of 82.6% at 30 d and a significant decrease in <0.25 mm soil aggregate particle size of 10.0% at 150 d, whereas the pig manure group had a significant increase in 1-0.5 mm particle size of 49.5% at 90 d. Application of different livestock manures did not significantly affect the geometric mean diameter (GMD) of soil particles, while it significantly affected the mean weight diameter (MWD) and macroaggregate mass fraction (WR > 0.25) of soil particles; WR > 0.25 in the chicken manure group was significantly higher by 10.3% at 150 d compared to the CK group; soil bulk weight decreased by 16.0% and 13.0% at 90 d compared to the CK in the chicken and cow dung groups, respectively; and capillary porosity in the chicken manure group was significantly higher by 50.0% at 60 d compared to the non-capillary porosity which decreased by 38.5%. Chicken manure, hog manure and cow manure significantly increased water content, field holding capacity and saturated water content compared to the CK group; at 90 d, field water holding capacity was significantly increased by 13.7%, 27.7% and 19.1% for hog manure, chicken manure and cattle manure applied compared to CK, respectively; soil water content increased by 9.8%, 21.3%, and 12.1%; soil saturated water content increased by 17.1%, 35.3%, and 26.7%, respectively. Compared with the CK group, the chicken, pig and cow manure groups showed an increase in initial infiltration of 6.2%, 20.5% and 17.9%, in stable infiltration of 1.7%, 23.9% and 4.0%, and in average infiltration of 15.4%, 38.3% and 18.4% at 90 d. The average infiltration of the chicken, pig and cow manure groups was higher than that of the CK group. In addition, correlation analyses showed a negative correlation between soil bulk weight and soil infiltration, soil water content, and soil porosity, and a positive correlation between GMD and MWD, and between soil infiltration and soil water content and soil porosity. In summary, the application of livestock manure can improve the physical properties of soil on black soil slopes cultivated land, and the application of chicken manure is more effective to improve the soil.
livestock manure / black soil slope cropland / soil physics / soil structure / improved soil {{custom_keyword}} /
| [1] |
韩晓增, 邹文秀. 我国东北黑土地保护与肥力提升的成效与建议[J]. 中国科学院院刊, 2018, 33(2):206-212.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [2] |
梁爱珍, 张延, 陈学文, 等. 东北黑土区保护性耕作的发展现状与成效研究[J]. 地理科学, 2022, 42(8):1325-1335.
东北黑土区承担着国家粮食安全“稳压器”的重要责任。然而，由于长期超负荷开发利用导致黑土日益退化，黑土资源的永续利用受到严重制约。理论与实践证明，保护性耕作是保护黑土地、推动黑土耕地质量和耕作效益绿色增长的发展模式。综述了保护性耕作的基本内涵及其在东北黑土区的发展现状与技术概况，从保护性耕作在土壤保持、保墒效益、结构改善、固碳培肥和土壤生物多样性增加、节本增效等方面系统评估了东北黑土区实施保护性耕作后的生态与经济效益，提出黑土区实施保护性耕作存在的问题与未来发展方向，以促进黑土地保护与利用协调发展、推动保护性耕作高质量跨越式发展。
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [3] |
王世豪, 徐新良, 黄麟, 等. 1980s-2010s东北农田土壤养分时空变化特征[J]. 应用生态学报, 2023, 34(4):865-875.
近年来,东北地区农田土壤“变薄、变瘦、变硬”等退化问题日趋严峻,严重影响了东北农业的可持续发展。本研究基于1980年代(1980s)《中国土种志》和2010年代(2010s)《中国土系志》土壤样点的土壤剖面属性数据,通过大样本统计分析,揭示了30年来东北不同地区、不同土壤类型的土壤养分状况变化规律。结果表明: 1)1980s—2010s,东北地区各土壤养分指标变化程度不同,土壤pH总体下降0.03,土壤有机质(SOM)含量下降最突出,下降了8.99 g·kg-1,降幅为23.6%,土壤全氮(TN)、全磷(TP)和全钾(TK)含量呈现出不同程度的上升趋势,增幅分别为17.1%、46.8%和4.9%。2)各省市土壤养分指标变化表现出较大差异,辽宁土壤酸化最明显,pH降低了0.32,SOM含量下降最明显,降低31.0%,土壤TN、TP、TK含量上升最显著,增幅分别为73.8%、248.1%和44.0%。3)不同土壤类型土壤养分变化差异较大,棕壤和栗钙土pH下降最多,几乎所有类型土壤的SOM含量均为下降趋势,其中棕壤、暗棕壤和黑钙土分别下降了35.4%、33.8%和26.0%,而TN、TP、TK含量上升最多的为棕壤,增幅分别为89.1%、232.8%和48.5%。综上,有机质含量下降和土壤酸化是1980s—2010s东北土壤退化的核心问题,探索合理的耕作方式,制定针对性的保护策略,是保证东北地区农业可持续发展的迫切需求。
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [4] |
邹文秀, 韩晓增, 陆欣春, 等. 不同土地利用方式对黑土剖面土壤物理性质的影响[J]. 水土保持学报, 2015, 29(5):187-193.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [5] |
王迎春, 杨黎, 王立刚. 黑土带土壤有机质研究进展[C]// 中国农业资源与区划学会.2015年中国农业资源与区划学会学术年会论文集.中国农业科学院农业资源与农业区划研究所, 2015:9.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [6] |
郝小雨, 马星竹, 周宝库. 长期单施有机肥黑土大豆产量和土壤理化性质演变特征[J]. 土壤与作物, 2018, 7(2):222-228.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [7] |
赵占辉, 张丛志, 蔡太义, 等. 不同稳定性有机物料对砂姜黑土理化性质及玉米产量的影响[J]. 中国生态农业学报, 2015, 23(10):1228-1235.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [8] |
刘晓林, 陈伟, 吴雅薇, 等. 秸秆颗粒改良剂对川西北高寒沙地土壤氮素和黑麦草生长的影响[J]. 水土保持学报, 2018, 32(6):229-235.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [9] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [10] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [11] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [12] |
孙万春, 周家昊, 俞巧钢, 等. 豆渣、猪粪有机肥施用水平对梨产量品质及土壤肥力的影响[J]. 果树学报, 2022, 39(9):1628-1638.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [13] |
候健勋, 张水梅, 袁静超, 等. 玉米秸秆源有机物料对黑土养分有效性与酶活性的提升效应[J]. 植物营养与肥料学报, 2021, 27(4):610-618.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [14] |
周连仁, 曾宪楠, 孟庆峰, 等. 不同培肥措施下盐碱旱地土壤肥力特征综合评价[J]. 东北农业大学学报, 2015, 46(6):34-39.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [15] |
王娜, 王璐, 宋昌海. 东北黑土区坡耕地土壤侵蚀及其治理研究进展[J]. 南方农业,. 2022, 16(17):160-162,166.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [16] |
张兴义, 李健宇, 郭孟洁, 等. 连续14年黑土坡耕地秸秆覆盖免耕水土保持效应[J]. 水土保持学报, 2022, 36(3):44-50.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [17] |
盖浩, 刘平奇, 张梦璇, 等. 黑土坡耕地横坡垄作对减少径流及土壤有机碳流失的作用[J]. 水土保持学报, 2022, 36(2):300-304.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [18] |
胡海清, 陆昕, 孙龙. 土壤活性有机碳分组及测定方法[J]. 森林工程, 2012, 28(5):18-22.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [19] |
亢晨波, 郭汉清, 张垚, 等. 复垦区不同土地利用类型土壤入渗特征及其影响因素[J]. 中国水土保持科学(中英文), 2023, 21(5):71-80.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [20] |
黄怡婷, 陈俊熹, 高钰淏, 等. 长期耕作对典型黑土水力性质的影响[J]. 土壤学报, 2024, 61(4):998-1008.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [21] |
徐军生. 克山县黑土区退化坡耕地综合治理技术研究[D]. 北京: 中国农业科学院, 2011.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [22] |
侯淑艳, 刘绪军, 刘建新, 等. 水土保持措施对黑土坡耕地产流产沙的影响[J]. 中国水土保持科学(中英文), 2022, 20(4):26-33.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [23] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [24] |
丛聪, 王天舒, 岳龙凯, 等. 深松配施有机物料还田对黑土区坡耕地土壤物理性质的改良效应[J]. 中国土壤与肥料, 2021(3):227-236.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [25] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [26] |
赵欣宇, 吴景贵, 刘文利, 等. 农业有机废弃物对黑土腐殖质元素组成的影响[J]. 水土保持学报, 2016, 30(02):301-306.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [27] |
张陆, 曹玉博, 王惟帅, 等. 鸡粪添加对蔬菜废弃物堆肥腐殖化过程的影响[J]. 中国生态农业学报(中英文), 2022, 30(2):258-267.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [28] |
魏宇轩, 蔡红光, 张秀芝, 等. 不同种类有机肥施用对黑土团聚体有机碳及腐殖质组成的影响[J]. 水土保持学报, 2018, 32(3):258-263.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [29] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [30] |
曾宪楠. 不同有机培肥措施对退化黑土肥力的影响[D]. 哈尔滨: 东北农业大学, 2014.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [31] |
刘殿民, 沈海鸥, 武佳龙, 等. 黑土坡面垄侧少耕措施的土壤侵蚀特征分析[J]. 水土保持学报, 2022, 36(4):1-6.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [32] |
李威闻, 黄金权, 齐瑜洁, 等. 土壤侵蚀条件下土壤微生物生物量碳含量变化及其影响因素的Meta分析[J]. 生态环境学报, 2023, 32(1):47-55.
土壤侵蚀是碳流失的重要驱动力，分析土壤侵蚀条件下土壤微生物生物量碳（SMBC）含量变化及其相关影响因素，对理解土壤侵蚀对土壤养分周转与碳循环机制具有重要意义。以未发生侵蚀为对照，基于2003—2022年间相关学者在中国区域内开展的有关土壤侵蚀对SMBC影响研究已公开发表的35篇学术论文的230组试验数据，按照土壤类型（紫色土、黑土、黄土和红壤）、土壤容重（高容重和低容重）、土地利用方式（林地、农田、草地和坡耕地）、水力侵蚀类型区（东北黑土区、西北黄土高原区、西南土石山区和南方红壤丘陵区）、年平均降雨量（1000—2000 mm、500—1000 mm和≤500 mm）和年平均温度（≥20 ℃、10—20 ℃、5—10 ℃和<5 ℃）进行分组，采用Meta分析对土壤侵蚀条件下SMBC含量变化的特征进行综合分析，并通过亚组分析探讨了侵蚀对SMBC的影响。研究发现，与未发生土壤侵蚀相比，（1）土壤侵蚀导致SMBC含量显著降低（下降程度为35.39%，置信区间为-0.4074— -0.3005）；（2）紫色土、黑土、黄土和红壤中，土壤侵蚀对SMBC含量的影响均表现出显著的负效应，下降幅度分别为78.72%、43.49%、42.52%和18.48%。不同土壤容重条件下，土壤侵蚀使SMBC含量显著下降，SMBC下降程度在高容重条件下是低容重的2.12倍。同时不同土地利用类型中林地（33.26%）SMBC下降最少，草地（39.73%）下降最多。SMBC含量的下降程度在东北黑土区（43.55%）最高，西北黄土高原区（42.57%）和西南土石山区（33.68%）次之，在南方红壤丘陵区（27.51%）最低；不同年均降雨量和不同年均温条件下的SMBC含量下降程度在年均降雨量1000—2000 mm、500—1000 mm和≤500 mm的地区分别为29.91%、43.15%和37.52%，在年均温为10—20 ℃、5—10 ℃和<5 ℃的地区分别为40%、37.25%和43.58%。由此可见，土壤侵蚀显著降低SMBC含量；不同土壤类型、不同土地利用方式、不同土壤容重、不同水力侵蚀类型区、不同年均降雨量等条件下，土壤侵蚀对SMBC下降的作用程度不同。
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [33] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [34] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [35] |
江恒. 有机物输入量对黑土结构性质及其季节性变化的影响[D]. 长春: 中国科学院大学(中国科学院东北地理与农业生态研究所), 2019.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [36] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [37] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [38] |
郝近羽, 刘瑾, 陈源泉, 等. 施用不同有机物料对砂质土壤玉米成熟期根际细菌群落变化的影响[J]. 中国农业大学学报, 2022, 27(10):65-79.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [39] |
王欢欢, 元野, 任天宝, 等. 生物炭对东北黑土理化性质影响研究[J]. 中国农学通报, 2018, 34(35):67-71.
为探明生物炭对我国黑土理化性质的影响,本研究通过大田试验,设置了设计5个处理,1个空白对照,每个处理0.06 hm2,共3个重复,分别为600 kg/hm2,1200 kg/hm2,1800 kg/hm2,2400 kg/hm2,3000 kg/hm2其依次定为T1、T2、T3、T4、T5,空白对照为CK。研究表明：在土壤物理性状方面,生物炭能够提高土壤空隙度、电导率以及持水量,同时降低土壤容重；在化学养分方面,生物炭能够有效提高土壤有机碳、破解氮、有效磷、有效钾的含量；在供试作物方面,生物炭能够有效提高根系活力以及总根尖数。总之,改善土壤物理结构以及其他物理性状,同时提高土壤养分含量,促进作物根系活力以及根尖数的提高,但对于生物炭对不同土壤作用的特点、施用量以及作用程度还有待进一步研究。
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [40] |
王笃超, 吴景贵. 不同有机物料对连作大豆土壤养分及团聚体组成的影响[J]. 土壤学报, 2018, 55(4):825-834.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [41] |
侯建勋, 张水梅, 袁静超, 等. 玉米秸秆源有机物料对黑土养分有效性与酶活性的提升效应[J]. 植物营养与肥料学报, 2021, 27(4):610-618.
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [42] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| [43] |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
| {{custom_ref.label}} |
{{custom_citation.content}}
{{custom_citation.annotation}}
|
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