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When agents thus constitute themselves without ambivalence (that is, unresolved desire for a thing and against it) or inconsistency (that is, unresolved desire for incompatible things), then the agent has what Frankfurt calls wholeheartedness.

当代理者这样地没有含糊其辞(即:对某样东西即赞成又反对的一个未解决的渴求)或不一致(即:对不互不相容事物的一个未解决的渴求)地构造出了他们自己,那么代理者拥有了Frankfurt称之为的全心全意。

For any initial generalized bisymmetric matrix $X_1$, when $AXB=C$ is consistent, we can obtain the generalized bisymmetric solution of the matrix equation AXB=C within finite iterative steps by the iteration method in the absence of roundoff errors; Moreover, the least-norm solution $X^*$ can be obtained by choosing a special kind of initial generalized bisymmetric matrix.

在不考虑机器误差的情况下,当矩阵方程AXB=C相容时,对任意广义双对称X_1,矩阵方程AXB=C的解可以经过有限步迭代得到;特别地,通过选择特殊地初始广义双对称矩阵极小范数解X^*。

Correspondingly, the abundances of incompatible elements in the first two formations is higher than those in the last formation, and the differences can be attributed to the different degrees of partial melting.

相应地,前者的不相容元素丰度普遍高於后者。两者之间的差异主要是部分熔融程度的差异所致。

Some geologists,however,on the basis of observations concerning mantle xenoliths, argue that the mantle is not layered,but that heterogeneity is created by fluids rich in "incompatible elements" percolating upward and transforming portions of the upper mantle irregularly,according to the vagaries of the fluids' pathways.

但是,某些地质学家,以对地幔捕虏岩体所作的观察为依据,指出地幔并非是分层排列的,相反,地幔的异质性是由那些富含&不相容成分&的流质构成的,这些成分趋向于流体而非固体的状态,自下而上渗透扩散,并依照这些流质流向的任意性,不规则地将上部地幔的某些部分予以改变。

Some geologists,however,on the basis of observations concerning mantle xenoliths,argue that the mantle is not layered,but that heterogeneity is created by fluids rich in "incompatible elements"(elements tending toward liquid rather than solid state)percolating upward and transforming portions of the upper mantle irregularly,according to the vagaries of the fluids'pathways.

但是,某些地质学家,以对地幔捕虏岩体所作的观察为依据,指出地幔并非是分层排列的,相反,地幔的异质性是由那些富含&不相容成分&的流质构成的,这些成分趋向於流体而非固体的状态,自下而上渗透扩散,并依照这些流质流向的任意性,不规则地将上部地幔的某些部分予以改变。

Some geologists,however,on the basis of observations concerning mantle xenoliths, argue that the mantle is not layered,but that heterogeneity is created by fluids rich in pathways.

但是,某些地质学家,以对地幔捕虏岩体所作的观察为依据,指出地幔并非是分层排列的,相反,地幔的异质性是由那些富含不相容成分的流质构成的,这些成分趋向于流体而非固体的状态,自下而上渗透扩散,并依照这些流质流向的任意性,不规则地将上部地幔的某些部分予以改变。

Lin argues that the threat of withdrawal from an agricultural collective by harder-working members helps discipline would-be shirkers. The removal of exit rights destroyed this self-enforcing discipline, reduced work incentives, and hence contributed to the fall in grain output.

林认为从农村集体合作社撤退意味着将受到其他人员的威胁和处罚,这种没有退出权的机制在某种程度上与所谓的&自我约束&纪律是不相容的,极大地降低了工作激励,因此才导致粮食的减产。

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