0.5mm)的含量,且土壤結(jié)構(gòu)的穩(wěn)定性顯著提高,,其作用深度在50cm以上,。②隨著土層的加深,,土壤總有機(jī)碳和活性有機(jī)碳均表現(xiàn)為先增加后降低再趨于穩(wěn)定的趨勢(shì),。免耕處理在0~80cm土層的土壤總有機(jī)碳和活性有機(jī)碳均高于常規(guī)耕作處理,。③隨著土層的加深,,不同粒級(jí)團(tuán)聚體總有機(jī)碳含量呈降低趨勢(shì),,大粒級(jí)團(tuán)聚體中含有較高的有機(jī)碳,。免耕更利于0~40cm土層不同粒級(jí)團(tuán)聚體總有機(jī)碳含量的提高,。隨著土壤團(tuán)聚體粒級(jí)的降低,土壤活性有機(jī)碳含量呈降低趨勢(shì),。與常規(guī)耕作相比,,除0.053~0.250mm粒級(jí)團(tuán)聚體外,免耕提高了0~20cm土層各粒級(jí)團(tuán)聚體中活性有機(jī)碳含量,。④隨著土層的加深,,各粒級(jí)團(tuán)聚體中有機(jī)碳對(duì)土壤總有機(jī)碳的貢獻(xiàn)率表現(xiàn)為先降低后增加再降低的趨勢(shì)。不同粒級(jí)團(tuán)聚體中,,大于2.0mm和小于0.053mm粒級(jí)團(tuán)聚體有機(jī)碳貢獻(xiàn)率在0~100cm土層均低于其他粒級(jí)團(tuán)聚體,。在0~20cm、30~40cm和90~100cm土層,,免耕處理各粒級(jí)團(tuán)聚體有機(jī)碳累積貢獻(xiàn)率均高于常規(guī)耕作,。"/>

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長(zhǎng)期免耕對(duì)不同土層土壤結(jié)構(gòu)與有機(jī)碳分布的影響
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國(guó)家自然科學(xué)基金項(xiàng)目(U1404404)、國(guó)家重點(diǎn)研發(fā)計(jì)劃項(xiàng)目(2017YFD0301102)和河南省農(nóng)業(yè)科學(xué)院優(yōu)秀青年科技基金項(xiàng)目(2016YQ12)


Effects of Long-term No-tillage on Soil Structure and Organic Carbon Distribution in Different Soil Layers
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    摘要:

    為探明長(zhǎng)期翻耕與免耕條件下不同土層深度土壤結(jié)構(gòu)穩(wěn)定性及其有機(jī)碳分布特征,在長(zhǎng)期定位試驗(yàn)中分層(0~10cm,、10~20cm,、…、90~100cm)采集免耕和常規(guī)耕作處理下混合土樣和原狀土樣進(jìn)行土壤結(jié)構(gòu)與有機(jī)碳的測(cè)定,,結(jié)果表明:①隨著土層的加深,,0.5~2.0mm和大于2.0mm粒級(jí)團(tuán)聚體含量表現(xiàn)為逐漸降低的趨勢(shì),而其他粒級(jí)團(tuán)聚體含量呈增加趨勢(shì),。免耕更利于提高大粒級(jí)團(tuán)聚體(>0.5mm)的含量,,且土壤結(jié)構(gòu)的穩(wěn)定性顯著提高,其作用深度在50cm以上,。②隨著土層的加深,,土壤總有機(jī)碳和活性有機(jī)碳均表現(xiàn)為先增加后降低再趨于穩(wěn)定的趨勢(shì)。免耕處理在0~80cm土層的土壤總有機(jī)碳和活性有機(jī)碳均高于常規(guī)耕作處理,。③隨著土層的加深,,不同粒級(jí)團(tuán)聚體總有機(jī)碳含量呈降低趨勢(shì),大粒級(jí)團(tuán)聚體中含有較高的有機(jī)碳,。免耕更利于0~40cm土層不同粒級(jí)團(tuán)聚體總有機(jī)碳含量的提高,。隨著土壤團(tuán)聚體粒級(jí)的降低,土壤活性有機(jī)碳含量呈降低趨勢(shì),。與常規(guī)耕作相比,,除0.053~0.250mm粒級(jí)團(tuán)聚體外,免耕提高了0~20cm土層各粒級(jí)團(tuán)聚體中活性有機(jī)碳含量,。④隨著土層的加深,,各粒級(jí)團(tuán)聚體中有機(jī)碳對(duì)土壤總有機(jī)碳的貢獻(xiàn)率表現(xiàn)為先降低后增加再降低的趨勢(shì)。不同粒級(jí)團(tuán)聚體中,,大于2.0mm和小于0.053mm粒級(jí)團(tuán)聚體有機(jī)碳貢獻(xiàn)率在0~100cm土層均低于其他粒級(jí)團(tuán)聚體,。在0~20cm、30~40cm和90~100cm土層,,免耕處理各粒級(jí)團(tuán)聚體有機(jī)碳累積貢獻(xiàn)率均高于常規(guī)耕作,。

    Abstract:

    In order to investigate the stability of soil structure and the distribution characteristics of organic carbon in different soil depths (0~10cm, 10~20cm,…, 90~100cm) under long-term conventional tillage and no-tillage conditions, mixed soil samples and undisturbed soil samples collected from no-tillage and conventional tillage treatments were designed to measure soil structure and soil organic carbon content. The results indicated that with the increase of soil depth, the contents of aggregates with diameter of 0.5~2.0mm and greater than 2.0mm were gradually decreased, while other particle agglomerates were increased. No-tillage treatment could improve the large aggregates (greater than 0.5mm) content, and significantly improve the stability of soil structure, the effect of depth was more than 60cm. With the increase of soil depth, soil organic carbon and active organic carbon content were increased firstly and then decreased, and then trended to be stable. Soil carbon and active organic carbon of no-tillage treatment in 0~80cm soil layer were higher than that of conventional tillage. With the increase of soil depth, soil aggregates organic carbon content was decreased, while organic carbon content of large aggregates was higher than other size aggregates. No-tillage was more conducive to increase soil organic carbon content of different size aggregates under 0~40cm soil depth. With the decrease of soil aggregates, soil active organic carbon content was decreased. Compared with conventional tillage, except 0.053~0.250mm size aggregate, no-tillage increased active organic carbon content in 0~20cm soil layer of various aggregates. With the increase of soil depth, the contribution rate of organic carbon to soil total organic carbon in different size fractions showed the trend of decreasing first, then increasing and then decreasing. In different aggregates, contribution rate of organic carbon of aggregates with diameter greater than 2.0mm and less than 0.053mm in the 0~100cm soil layer was lower than those of other size aggregates. In 0~20cm, 30~40cm and 90~100cm soil layers, accumulation contribution rate of different aggregates organic carbon of no-tillage treatment was higher than that of conventional tillage.

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楊永輝,武繼承,丁晉利,張潔梅,潘曉瑩,何方.長(zhǎng)期免耕對(duì)不同土層土壤結(jié)構(gòu)與有機(jī)碳分布的影響[J].農(nóng)業(yè)機(jī)械學(xué)報(bào),2017,48(9):173-182. YANG Yonghui, WU Jicheng, DING Jinli, ZHANG Jiemei, PAN Xiaoying, HE Fang. Effects of Long-term No-tillage on Soil Structure and Organic Carbon Distribution in Different Soil Layers[J]. Transactions of the Chinese Society for Agricultural Machinery,2017,48(9):173-182.

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  • 收稿日期:2017-05-03
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  • 在線發(fā)布日期: 2017-09-10
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