2) soil organic carbon mineralization
土壤有机碳矿化
1.
Effects of environmental factors on soil organic carbon mineralization in a Pinus sylvestris var.mongolica plantation.;
不同环境因子对樟子松人工林土壤有机碳矿化的影响
2.
Soil organic carbon mineralization was mainly influenced by the content of soil organic carbon,microbial biomass carbon and dissolved organic carbon,and the correlation coefficients were 0.
结果表明,水田、旱地土壤有机碳矿化规律均表现为培养前期快速下降,培养后期保持相对稳定的趋势,符合对数关系。
3) Potentially mineralized C
土壤潜在可矿化有机碳
1.
Potentially mineralized C (C0), easily mineralized C (C1) and the initial potential rate of C mineralization (C0k) were significantly different among the treatments with a general decline order of organic manure treatments>mineral fertilizer treatments>control, which were positively correlated to soil organic carbon, total nitrogen and microbial activity.
拟合所得土壤潜在可矿化有机碳量(C0)、易矿化有机碳量(C1)和初始潜在矿化速率(C0k)均表现出有机肥处理高于化肥处理,施肥处理高于不施肥处理(NK处理除外),与土壤有机碳、全氮和土壤微生物活度均呈显著正相关;有机碳矿化速率(k)和土壤潜在可矿化有机碳占土壤总有机碳的比例在处理间差异均不显著,除k与有机碳呈显著负相关外,其他与土壤性质均无显著相关性。
5) mineralisable nitrogen potential
土壤矿化势
1.
AOL in treatment with sand showed a higher percentage of nitrogen was mineralized than that of without sand, and so was the mineralisable nitrogen potential in the soil.
在相同的时间里加砂处理比未加砂的氮素矿化量大,并且加砂处理可以显著提高施入AOL后的土壤矿化势,表明改善通气状况可以提高土壤有机质的矿化强度和供氮潜力。
6) mineralization of soil nitrogen
土壤氮矿化
1.
The mineralization of soil nitrogen and its influenced factors under alpine meadows in Qilian Mountains;
祁连山中部高寒草甸土壤氮矿化及其影响因素研究
补充资料：土壤有机胶体
分子式：
CAS号：
性质：又称腐殖质胶体(humus colloid)，由土壤中动植物残体经微生物分解后又重新合成的产物所组成。主要有腐殖质，也有一些木质素、蛋白质、纤维素、树脂等化合物。
CAS号：
性质：又称腐殖质胶体(humus colloid)，由土壤中动植物残体经微生物分解后又重新合成的产物所组成。主要有腐殖质，也有一些木质素、蛋白质、纤维素、树脂等化合物。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条