Zou Wen-Xiu, Han Xiao-Zeng, Lu Xin-Chun, Chen Xu, Yan Jun, Song Bao-Hui, Yang Ning, Lin Qing-Hua, He Yu
Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Harbin 150081, China.
Liaoning Province Modern Agricultural Production Base and Construction Engineering Center, Shenyang 111000, China.
Ying Yong Sheng Tai Xue Bao. 2020 Dec;31(12):4134-4146. doi: 10.13287/j.1001-9332.202012.030.
Organic amendment return could enhance soil fertility, improve soil structure, and increase crop yield. However, how construction of soil layers can affect soil fertility and crop yield are not fully understood. We examined the effects of constructions of fertile and cultivated soil layer on soil fertility and maize yield in the upland black soil region in Northeast China, to provide theoretical guidance in increasing soil fertility and sustainable development of agriculture. Based on the combination of field plot experiments and demonstration regions, nine study sites with different ecological characteristics were selected from Heilongjiang, Jilin and Liaoning provinces from northeast China, covering dark brown, black, meadow, chernozem, albic, brown and cinnamon soils. There were three treatments in each study site, including maize straw return within 0-35 cm soil layer (CF), the combination of maize straw and organic manure return within 0-35 cm soil layer (CF) and conventional agricultural practice without organic amendmentas control (CK). The rate of straw return in CF and CF treatments were 10000 kg·hm, and full straw for demonstration regions. The rate of organic manure in CF treatment was 30000 kg·hm. Considerable difference in soil fertility were recorded among the nine study sites with the trend of tillage layer > sub-tillage layer, especially for dark brown soil and albic soil. Soil fertility of tillage layer and sub-tillage layer was relatively low both for brown soil and cinnamon soil. The heavy clay and plow pan were pivotal limiting factors of soil fertility for the black soil and the meadow soil. Compared with CK, the concentrations of soil organic matter (SOM), available nitrogen (AN), available phosphorous (AP), and available potassium (AK) in tillage layers was increased on average by 1.85 g·kg, 20.16 mg·kg, 1.56 mg·kg and 17.2 mg·kg in the CF and CF treatments in five study sites with more than two years of treatments. The contents of SOM, AN, AP and AK in sub-tillage layer increased by 2.09 g·kg, 12.06 mg·kg, 2.18 mg·kg and 3.84 mg·kg, compared with tillage layer. CF treatment significantly enhanced the contents of SOM and AP in both tested soil layers, while CF treatment significantly enhanced all fertility indices in both tested soil layers. This indicated that the increase of organic amendment return is an effective way to improve soil fertility. Maize yield fluctuated under the combined effect of climatic conditions and soil types. The significant differences in maize yield under CK, CF and CF treatments were observed with a trend of CF > CF > CK. This result indicated that the construction of fertile and cultivated soil layer could significantly increase maize yield independent of soil types. The construction of fertile and cultivated soil layer based on maize straw return or maize straw and organic manure combined return within 0-35 cm soil layer, could simultaneously increase soil fertility in both tillage and sub-tillage layer, as well as maize yield. We suggested that the selection of approaches of the constructions of fertile and cultivated soil layer should consider soil types and the sources of organic amendments. It should also give priority to soil layers rich in organic manure source to construct fertile and cultivated soil layers.
有机物料还田能够提高土壤肥力、改善土壤结构并增加作物产量。然而,土层构建如何影响土壤肥力和作物产量尚未完全明晰。我们研究了肥沃耕作土层构建对中国东北旱地黑土区土壤肥力和玉米产量的影响,旨在为提高土壤肥力及农业可持续发展提供理论指导。基于田间小区试验与示范区相结合的方式,从中国东北的黑龙江、吉林和辽宁三省选取了9个具有不同生态特征的研究地点,涵盖暗棕壤、黑土、草甸土、黑钙土、白浆土、棕壤和褐土。每个研究地点设置了3种处理,包括0 - 35厘米土层内玉米秸秆还田(CF)、0 - 35厘米土层内玉米秸秆与有机肥联合还田(CF)以及不进行有机物料添加的传统农业做法作为对照(CK)。CF和CF处理的秸秆还田量为10000千克·公顷,示范区为全量秸秆。CF处理的有机肥用量为30000千克·公顷。9个研究地点的土壤肥力存在显著差异,呈现耕作层>亚耕作层的趋势,尤其是暗棕壤和白浆土。棕壤和褐土的耕作层和亚耕作层土壤肥力相对较低。重黏土和犁底层是黑土和草甸土土壤肥力的关键限制因素。与CK相比,在经过两年以上处理的5个研究地点,CF和CF处理的耕作层土壤有机质(SOM)、碱解氮(AN)、有效磷(AP)和速效钾(AK)含量平均分别增加了1.85克·千克、20.16毫克·千克、1.56毫克·千克和17.2毫克·千克。与耕作层相比,亚耕作层的SOM、AN、AP和AK含量分别增加了2.09克·千克、12.06毫克·千克、2.18毫克·千克和3.84毫克·千克。CF处理显著提高了两个测试土层中SOM和AP的含量,而CF处理显著提高了两个测试土层中的所有肥力指标。这表明增加有机物料还田是提高土壤肥力的有效途径。玉米产量在气候条件和土壤类型的综合作用下波动。在CK、CF和CF处理下,玉米产量存在显著差异,呈现CF>CF>CK的趋势。这一结果表明,肥沃耕作土层的构建能够显著提高玉米产量,且不受土壤类型的影响。基于0 - 35厘米土层内玉米秸秆还田或玉米秸秆与有机肥联合还田构建肥沃耕作土层,能够同时提高耕作层和亚耕作层的土壤肥力以及玉米产量。我们建议,肥沃耕作土层构建方法的选择应考虑土壤类型和有机物料来源。还应优先选择有机物料来源丰富的土层来构建肥沃耕作土层。