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耕地利用轉(zhuǎn)型碳排放時空分異特征與形成機理研究
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國家自然科學基金項目(41461040)、黑龍江省自然科學基金項目(LH2019D012)和東農(nóng)學者計劃項目(19QC37)


Spatio-temporal Differentiation Characteristics and Formation Mechanism of Carbon Emission from Cultivated Land Use Transformation
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    摘要:

    為揭示耕地利用轉(zhuǎn)型的碳排放時空分異特征,以松花江流域哈爾濱段為例,基于網(wǎng)格單元法和碳排放系數(shù),測度1990—2020年耕地利用轉(zhuǎn)型的碳排放強度,并借助重心分析、探索性空間數(shù)據(jù)分析、冷熱點分析工具和地理探測器等研究方法揭示耕地利用轉(zhuǎn)型的碳排放空間異質(zhì)性與形成機理。結(jié)果表明:1990—2020年耕地面積呈下降趨勢,耕地與建設(shè)用地、林地之間的轉(zhuǎn)型最為劇烈,耕地主要轉(zhuǎn)型為建設(shè)用地。1990—2020年耕地利用轉(zhuǎn)型碳排放量呈上升趨勢,由1990—2000年的3704.12t增加到2010—2020年的35656.29t,增加了近8.63倍,耕地利用轉(zhuǎn)型碳排放最終呈現(xiàn)為碳源形式。1990—2020年耕地利用轉(zhuǎn)型碳排放重心基本保持穩(wěn)定,向東移動了15.17km,其中1990—2010年重心移動距離最大,呈現(xiàn)東北地區(qū)碳排放惡化,而西南地區(qū)碳排放明顯改善的特點。1990—2020年耕地利用轉(zhuǎn)型碳排放非隨機分布,具有較強的空間集聚性,熱點區(qū)主要圍繞南崗區(qū)向周圍邊界擴散,冷點區(qū)零星點狀分布在東南部地區(qū)。與城鎮(zhèn)中心距離是耕地利用轉(zhuǎn)型碳排放的主控因子,各因子之間交互作用以雙因子增強為主,其中土地利用程度與年平均降水量、與城鎮(zhèn)中心距離之間的相互作用解釋力較強,耕地利用轉(zhuǎn)型碳排放空間分異特征是多因子共同作用的結(jié)果。

    Abstract:

    In order to reveal the temporal and spatial differentiation characteristics of carbon emissions from cultivated land use transition, taking Harbin section of Songhua River Basin as an example,the carbon emission intensity of cultivated land use transition from 1990 to 2020 was measured based on the grid element method and carbon emission coefficient. In addition, the means of gravity center analysis, exploratory spatial data analysis, cold and hot spot analysis tools and geodetector were implemented to reveal the spatial heterogeneity and formation mechanism of carbon emissions from cultivated land use transition. The results showed that the cultivated land area demonstrated a downward trend in 1990—2020, and the conversion between cultivated land and construction land, forest land was the most dramatic, and cultivated land mainly converted into construction land.The carbon emission of cultivated land use transformation showed an upward trend in 1990—2020, from 3704.12t in 1990—2000 to 35656.29t in 2010—2020 with an increase of nearly 8.63 times. The carbon emission of cultivated land use transformation eventually appeared as a carbon source. From 1990 to 2020, the carbon emission center of arable land use transformation remained basically stable, moving 15.17km to the east, of which the center of gravity moved the longest from 1990 to 2010. Overall the carbon emissions in the northeast region continue to deteriorate, while the carbon emissions in the southwest region were improved significantly. In 1990—2020, the carbon emissions from cultivated land use transformation were non randomly distributed, but had strong spatial agglomeration. The hot spots mainly spread around Nangang District to the surrounding boundary, and the cold spots were scattered in the southeast. Urban center distance was the main factor of carbon emission for cultivated land use transformation, and the interaction between various factors was mainly enhanced by two factors. Among them, the interaction between land use degree, and annual average precipitation, urban center distance had strong explanatory power. The spatial differentiation characteristics of carbon emission for cultivated land use transformation were the result of multi-factor interaction.

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蓋兆雪,詹汶羲,王洪彥,杜國明.耕地利用轉(zhuǎn)型碳排放時空分異特征與形成機理研究[J].農(nóng)業(yè)機械學報,2022,53(7):187-196. GAI Zhaoxue, ZHAN Wenxi, WANG Hongyan, DU Guoming. Spatio-temporal Differentiation Characteristics and Formation Mechanism of Carbon Emission from Cultivated Land Use Transformation[J]. Transactions of the Chinese Society for Agricultural Machinery,2022,53(7):187-196.

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  • 收稿日期:2021-08-08
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  • 在線發(fā)布日期: 2022-07-10
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